<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Wednesday. One small (size 1) slab and a few loose dry avalanches were triggered in steep terrain on Monday. A few size 1 wind slab avalanches were triggered by skiers over the weekend. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed on Wednesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed on Wednesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A size 1.5 windslab was triggered on a lee slope in the north of the region on Tuesday. It released on the weaker facets below the wind affected snow. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">A few thin (size 1) wind slabs were observed on Saturday, as well as numerous loose dry avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were preliminary reports of size 1-1.5 loose avalanches, and size 1 human triggered storm slab avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday there was one size 1 human triggered persistent slab avalanche reported on a north aspect at 1100 m. It failed on the late January persistent weak layer, 40 cm deep and was triggered remotely (from a distance).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Generally speaking, reports from the past week are mainly of wind slabs reacting to ski cuts, with a trend toward smaller (size 1) releases. Small (size 1-1.5) loose dry avalanches have also been observed releasing naturally from steeper, sun exposed slopes in recent days.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports of human triggered persistent slab avalanches on the January weak layers have been on the decline, suggesting these layers have evolved into a lower likelihood/high consequence avalanche problem.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region over the past few days, but observations in neighbouring regions have shown small (size 1) wind slabs reacting to skier traffic at upper elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity on the mid January persistent weak layer has tapered off, however test results still suggest that this layer could be triggered by humans in isolated terrain features such as steep cutblocks, and large, steep, open glades. This weak layer has become a low likelihood/high consequence scenario. Check out a recent MIN report from Allen Creek </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c332dad3-2584-4ef7-b639-03afd1c32762" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> that illustrates this.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed on Wednesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 slab avalanche on a north aspect was observed in the Highwood area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no reports of avalanche activity in the past few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were preliminary reports of a natural wind slab avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were several reports of human triggered wind slab, storm slab and loose snow avalanches, size 1-1.5, and natural loose and storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, a size 2 persistent slab avalanche was triggered by a cornice failure on a southeast aspect in the alpine. This avalanche reportedly failed on the late-January persistent weak layer.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Persistent slab avalanche activity on the buried surface hoar layers (described in more detail in the Snowpack Summary) has tapered significantly. This has evolved into a low likelihood avalanche/high consequence avalanche problem at treeline and below. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday and Thursday there were reports of several size 1 loose snow avalanches from steep terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of human triggered persistent slab avalanches that failed on the early February persistent weak layer (described in more detail in the Snowpack Summary). These were size 1 and 1.5, on west aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports of persistent slab avalanches are becoming less frequent, suggesting the January/February weak layers have evolved into a lower likelihood/high consequence avalanche problem.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Friday. Small loose wet avalanches are likely on south-facing slopes. Slab avalanches are likely to be confined to extreme terrain features under current conditions.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small storm slab and loose dry avalanches were triggered naturally, by skiers, and explosives on Thursday within the recent snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small (size 1) loose and slab avalanches were triggered naturally and by skiers on Thursday within the recent storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Two small (size 1.5) slab avalanches were triggered by separate ski groups on Thursday, one on a northwest aspect at 1250 m and one on a northwest aspect at 1500 m. Both are thought to have released on the mid-february weak layer buried 30-50 cm below the surface.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche have been reported from this region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were preliminary reports of human triggered storm slab avalanches up to size 2. There were also reports of a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few human triggered size 1 storm slab and loose snow avalanches. There were also a few reports of explosives triggered avalanches size 2-2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday there was one size 1 persistent slab avalanche reported on a north aspect at 1100 m. It failed on the late January persistent weak layer, 40 cm deep and was triggered remotely (from a distance).</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region recently.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small (size 1) loose dry avalanches were observed in treeline and alpine terrain on Thursday, being triggered naturally and by skiers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new today, but skies were obscured most of the day. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small loose dry avalanches were triggered by skiers within the recent storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of natural and human triggered avalanches to size 2, as well as a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were several reports of human triggered wind slab, storm slab and loose snow avalanches, size 1-1.5, and natural loose and storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of several natural and explosives triggered avalanches to size 2.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday and Thursday there were reports of several size 1 loose snow avalanches from steep terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of human triggered persistent slab avalanches that failed on the early February persistent weak layer (described in more detail in the Snowpack Summary). These were size 1 and 1.5, on west aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Friday. Small loose wet avalanches are likely on south-facing slopes. Small dry loose avalanches are likely on steep terrain elsewhere. Slab avalanches are likely to be confined to extreme terrain features under current conditions.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, several small (size 1) storm slab and loose dry avalanches were triggered naturally and by skiers within the recent snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, a few small (size 1) loose and slab avalanches were triggered naturally and by skiers within the recent storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported Friday. Two small (size 1.5) slab avalanches were triggered by separate ski groups on Thursday, one on a northwest aspect at 1250 m and one on a northwest aspect at 1500 m. Both are thought to have released on the mid-february weak layer buried 30-50 cm below the surface.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche have been reported from this region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were  reports of human triggered storm slab avalanches up to size 2. There were also reports of a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few human triggered size 1 storm slab and loose snow avalanches. There were also a few reports of explosives triggered avalanches size 2-2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday there was one size 1 persistent slab avalanche reported on a north aspect at 1100 m. It failed on the late January persistent weak layer, 40 cm deep and was triggered remotely (from a distance).</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of natural and human triggered loose snow avalanches size 1-1.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small loose dry avalanches were reported on Saturday. On Friday, numerous small (size 1) loose dry avalanches were observed in treeline and alpine terrain, being triggered naturally and by skiers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few new slides up to size 2.0 occurred in the past 24 hours, with the common denominators being N to E aspects, steep Alpine terrain, with fracture depths between 10 and 40cm. Some small solar triggered sluffs were also observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, small loose dry avalanches were triggered by skiers within the recent storm snow (see an example in this MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/ec3ec5a0-1fcb-47a1-87b7-7b71a4c2ef5f" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">). Since then the storm snow has likely settled and bonded to the underlying snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5. There was also a report of a remotely (from a distance) triggered size 2 persistent slab avalanche on a north aspect at 2300m in the south of the region. It was suspected to have run on a buried layer of facets.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of natural and human triggered avalanches to size 2, as well as a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of several natural and explosives triggered avalanches to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Friday or Saturday. Small loose wet avalanches are likely on south-facing slopes. Small dry loose avalanches are likely on steep terrain elsewhere. Slab avalanches are likely to be confined to extreme terrain features under current conditions.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, several small (size 1) storm slab and loose dry avalanches were triggered naturally and by skiers within the recent snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, a few small (size 1) loose and slab avalanches were triggered naturally and by skiers within recent storm snow. On Saturday, one size 2 wind slab avalanche was triggered by a skier north of Pemberton. The avalanche occurred on a southwest aspect at 1850 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanches suggest the incoming storm may produce bigger avalanches than might otherwise be expected because of the relatively weak, sugary facets the new storm snow is falling on.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday a small slab avalanche (size 1.5) was triggered in the facets releasing about 40 cm deep near treeline near Terrace. It didn't release wide, and didn't even run far (30 m). Two small (size 1.5) slab avalanches were triggered on Thursday, Both are thought to have released on the mid-february weak layer buried 30-50 cm below the surface.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche have been reported from this region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of human triggered storm slab avalanches up to size 2. There were also reports of a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Expect the likelihood of triggering storm and wind slab avalanches to increase as new snow accumulates on Monday. On Friday, there were reports of natural and human triggered loose dry avalanches size 1-1.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small loose dry avalanches were reported on Saturday. On Friday, numerous small (size 1) loose dry avalanches were observed in treeline and alpine terrain, being triggered naturally and by skiers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One new slide observed in Miner's Gully in the Bow Valley.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanche activity has been limited to small slab and loose avalanches in the top 20 cm of snow (size 1). Check recent MIN reports for some examples </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/17f3e223-fe24-4e5f-91e3-42fcacdcff24" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> and </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/ec3ec5a0-1fcb-47a1-87b7-7b71a4c2ef5f" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. Looking ahead, the most likely problem will be storm slabs that form with the incoming storm, however the lingering persistent weak layer in the North Shore Mountains still poses a low likelihood - high consequence problem.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday and Sunday. include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday there was a skier triggered size 2 persistent slab avalanche on a west aspect at 2300m in the north part of the region as well as a remotely triggered (from a distance) size 3 avalanche on a southwest aspect in the alpine. The second avalanche was in the south part of the region. Both of these were suspected to have run on a layer of facets.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There was also a report of a remotely triggered size 2 persistent slab avalanche on a north aspect at 2300m in the south of the region on Saturday. It was suspected to have run on a buried layer of facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Sunday indicate natural and human triggered storm and wind slab avalanches to size 1.5 on north and southwest aspects in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Friday or Saturday. Small loose wet avalanches are likely on south-facing slopes. Small dry loose avalanches are likely on steep terrain elsewhere. Slab avalanches are likely to be confined to extreme terrain features under current conditions.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Several small (size 1) loose dry and wet avalanches were reported over the weekend. Looking ahead, storm slab activity is expected with the new snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Several size 1-1.5 loose dry avalanches were reported over the weekend. See this MIN report for an example </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/49c5afb1-ebbb-43c5-be72-4df9ee03ffdf" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. On Saturday, a size 2 wind slab avalanche was triggered by a skier north of Pemberton. The avalanche occurred on a southwest aspect at 1850 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Initial reports from the field today (Monday) suggest whumpfing, cracking, remotely triggered avalanches, and a widespread avalanche cycle on Monday morning. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche have been reported from this region. However, I expect recent natural storm and wind slab up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Expect the likelihood of triggering storm and wind slabs to increase with new snow from Monday and Monday night. Reports on Saturday and Sunday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of human triggered storm slab avalanches up to size 2. There were also reports of a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Expect the likelihood of triggering storm and wind slab avalanches to increase as new snow has accumulated Monday into Tuesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small loose dry avalanches were reported over the weekend. One large (size 3) slab avalanche was triggered remotely on a southwest aspect on Sunday. The avalanche failed on a crust layer 20-30 cm deep, but showed surprisingly wide propagation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Few new slab avalanches  were observed on SW to NE faces .</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity over the weekend was limited to small slab and loose avalanches in the top 20 cm of snow (size 1). Looking ahead, the most likely problem will be fresh storm slabs, however the lingering persistent weak layer in the North Shore Mountains still poses a low likelihood - high consequence problem.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were preliminary reports of natural and explosives triggered storm slab avalanches up to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of numerous human triggered storm slab avalanches up to size 1.5 and several natural storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday and Sunday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Also on Sunday, was a skier triggered size 2 persistent slab avalanche on a west aspect at 2300m in the northern part of the region as well as a remotely triggered (from a distance) size 3 avalanche on a southwest aspect in the alpine. The second avalanche was in the south part of the region. Both of these were suspected to have run on a layer of facets.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There was a report of a remotely triggered size 2 persistent slab avalanche on a north aspect at 2300m in the south of the region on Saturday. It was suspected to have run on a buried layer of facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were preliminary reports of several size 1 human triggered storm slab and loose snow avalanches, as well as natural and explosives triggered loose snow avalanches up to size 2.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of a few size 1 human triggered storm slab avalanches, and one natural size 2 wind slab avalanche on a northwest aspect at 2600 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there were reports of natural and human triggered storm and wind slab avalanches to size 1.5 on north and southwest aspects in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Small and isolated (size 1) wind slab avalanches were naturally triggered Monday on steep alpine features. With this new round of precipitations and wind, storm and wind slabs are likely to be reactive on heavily wind exposed terrain at treeline and alpine, where small loose dry avalanches are likely on steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Small and isolated (size 1-1.5) wind slab avalanches were naturally and human triggered Monday on steep alpine features. Storm and wind slabs are likely to be develop on exposed terrain at treeline and alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Several small (size 1) loose dry and wet avalanches were reported over the weekend. Natural avalanche activity may remain possible on slopes affected by the sun.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Several size 1-1.5 loose dry avalanches were reported over the weekend. See this MIN report for an example </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/49c5afb1-ebbb-43c5-be72-4df9ee03ffdf" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. On Saturday, a size 2 wind slab avalanche was triggered by a skier north of Pemberton. The avalanche occurred on a southwest aspect at 1850 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">One size 2 windslab in the north of the region is worth noting: it was remotely triggered from 100 m away suggesting some sort of a persistent slab structure that won't heal overnight.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">In the south part of the region clouds limited observations but avalanche reports include numerous natural size 2 avalanches on all kinds of terrain 35 degrees or steeper, numerous remotely triggered size 2 slides. I suspect we'll learn more when the visibility improves and people see more terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Few observers in the field Monday but reports are consistent with a natural avalanche cycle of storm slabs and wind slab up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were preliminary reports of natural and explosives triggered storm slab avalanches up to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of human triggered storm slab avalanches up to size 1.5 and natural storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday and Sunday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of human triggered storm slab avalanches up to size 2. There were also reports of a natural avalanche cycle to size 2.5 in the neighboring Glacier National Park region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Expect to find reactive storm slabs at upper elevations, especially in wind loaded areas and on steep, sun-exposed slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in the region on Monday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small loose dry avalanches were reported over the weekend and into Monday. One large (size 3) slab avalanche was triggered remotely on a southwest aspect on Sunday. The avalanche failed on a crust layer 20-30 cm deep, but showed surprisingly wide propagation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A small natural avalanche cycle has occurred over the past 24 to 36 hours with thin wind slabs up to size 2.0 failing on all aspects in steeper terrain in the Alpine and Treeline elevation bands.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity over the weekend was limited to small slab and loose avalanches in the top 20 cm of snow (size 1). Looking ahead, the most likely problem will be fresh storm slabs. However the lingering persistent weak layer in the North Shore Mountains still poses a low likelihood - high consequence problem.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were reports of numerous natural and explosives triggered avalanches up to size 2, as well as human triggered storm slab avalanches up to size 1.5. Some of these were remoted triggered (triggered from a distance).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There was also a report of a size 2 human triggered persistent slab avalanche on a southeast aspect at treeline. It is suspected that this avalanche failed on the early February persistent weak layer.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of numerous human triggered storm slab avalanches up to size 1.5 and several natural storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday and Sunday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Also on Sunday, was a skier triggered size 2 persistent slab avalanche on a west aspect at 2300m in the northern part of the region as well as a remotely triggered (from a distance) size 3 avalanche on a southwest aspect in the alpine. The second avalanche was in the south part of the region. Both of these were suspected to have run on a layer of facets.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were preliminary reports of several natural and explosives triggered wind slab avalanches up to size 2, and a few human triggered loose snow avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were reports of several size 1 human triggered wind slab and loose snow avalanches, as well as natural and explosives triggered loose snow avalanches up to size 2.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of a few size 1 human triggered wind slab avalanches, and one natural size 2 wind slab avalanche on a northwest aspect at 2600 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Several small (up to size 1.5) storm slabs avalanches (natural and skier triggers) were reported Tuesday in the Lizard Range. With this recent round of precipitations, storm slabs are likely to be remain reactive on exposed terrain at treeline and alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Very few avalanches were reported lately due to limited visibility which did not allow for great assessment and / or travel. Few small loose dry avalanches (natural and skiers triggers) were reported on steep alpine slopes around Crowsnest. With recent precipitation and wind, wind slabs are likely to be reactive on exposed terrain at treeline and alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small loose wet avalanches were reported on Tuesday on south-facing slopes. There was also a size 1.5 remote-triggered avalanche reported at 1400 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">During the previous storm, there was an avalanche cycle to size 2.5. Operators noted some avalanches showed wide propagations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/330f213d-8a1e-47f0-a27b-1d39216f7327" target="_blank"><span class="s_B5813F7D">This avalanche</span></a><span class="s_3FE45715"> was reported from the Duffey Lake area on Tuesday. It indicates the nature of the bond between the recent storm snow and old surfaces below may be poor. Most other recent reports from this region have been of small loose snow avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">One size 2 wind slab in the north of the region is worth noting: it was remotely triggered from 100 m away suggesting some sort of a persistent slab structure that won't heal overnight.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">In the south part of the region clouds limited observations but avalanche reports include numerous natural size 2 avalanches on all kinds of terrain 35 degrees or steeper, numerous remotely triggered size 2 slides. I suspect we'll learn more when the visibility improves and people see more terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Few observers in the field Monday but reports are consistent with a natural avalanche cycle of storm slabs and wind slab up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were numerous reports of natural and explosives triggered avalanches up to size 2.5, as well as human triggered storm slab avalanches up to size 1.5. Some of these were remoted triggered (triggered from a distance).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of human triggered storm slab avalanches up to size 1.5 and natural storm slab avalanches up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Saturday and Sunday include several natural and human triggered storm slab, loose dry and wind slab avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were reports of several human triggered avalanches up to size 2. A few of these were triggered remotely (from a distance). There were also several reports of natural storm slab avalanches up to size 3. These avalanches occurred on all aspects and at all elevation bands.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Numerous small (size 1-1.5) storm slabs avalanches were triggered by skiers as well as few large ones (size 2-2.5) from explosives in alpine features on various aspects recently. One report mentioned a small slide triggered on a persistent weak layer about 65 cm down on southeast slope around 2000m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread loose dry avalanches up to size 1.5 in Alpine areas of the Eastern Ranges due to the recent fresh snow. There has also been very isolated thin wind slab activity up to size 1.5 in Alpine and Treeline terrain. Further west, there was little to no avalanche activity observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive control produced small (size 1) slab avalanches on Tuesday. No other avalanches were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3428770D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 15.3333333333333px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3428770D">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on primarily solar aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 50 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.</span><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, numerous naturally triggered wind slab avalanches up to size 2.5 and a few human triggered wind slabs up to size 1.5, were reported primarily on easterly aspects at treeline and above.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_702CA62 { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 14px;color: #000000; } 
.s_94A968CE { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 14px;color: #0000FF;text-decoration: underline; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_702CA62">On Thursday, a group of sledders remotely triggered a size 1.5 persistent slab after seeing many shooting crack and whumpfs. See the </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_94A968CE">MIN</span></a><span class="s_702CA62"> report for more details. </span><span class="s_A95EAA36">Wednesday, numerous storm slabs avalanches (size 1-2) were triggered by skiers on northerly aspects near ridgetops. Few larger loose dry avalanches (size 2-2.5) were also triggered by explosives on steep alpine slopes. Thursday, the sun has initiated several loose wet avalanches on solar aspects at treeline and above. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">On Wednesday, riders have triggered small storm slabs avalanches (up to size 1.5) on north facing slopes near ridgetops and few natural loose dry were observed on alpine feature. Also, small wind slabs were triggered on unexpected areas on lee slopes last few days. Sledders were surprised to remotely trigger a persistent slab avalanche down 60 cm late afternoon Thursday on a west facing slope below treeline. See the Min report form Lizard Range and Flathead for more details.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Wednesday was an active day for avalanche activity. Loose wet releases were common on steep solar aspects to size 2. This </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/cc13ff18-183f-40d6-8fa1-c3a8326a28bb" target="_blank"><span class="s_B5813F7D">MIN from Decker Meadows</span></a><span class="s_3FE45715"> does a great job of showing just how quickly the very strong spring sun can produce avalanches with some great photos and a positive outcome. We suspect activity like that </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/6fdec7a5-7aee-46ac-8f50-8150f142cb08" target="_blank"><span class="s_B5813F7D">described in this MIN</span></a><span class="s_3FE45715"> will probably pick up over the next few days as the region warms considerably. A size 2 natural wind slab avalanche was reported from a north facing feature at 1900 m. A size 1 remote triggered storm slab avalanche was also reported from a north facing feature between 2200 and 2000 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Small loose wet avalanches were reported on Tuesday on south-facing slopes. There was also a size 1.5 remote-triggered avalanche reported at 1400 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">During the previous storm, there was an avalanche cycle to size 2.5. Operators noted some avalanches showed wide propagations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday a skier remote triggered a size 2 wind slab on a northeast facing alpine slope at 2000 m with a crown 40 cm in depth. There are some great photos in </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1f8369e8-4b9c-4f02-a3ac-7658f17dd527" target="_blank"><span class="s_B5813F7D">this MIN</span></a><span class="s_3FE45715"> of a size 2.5 wind slab that was skier triggered on a north facing slope on the Slalok/Matier Glacier.  As we enter a period that looks to be increasingly warm it's worth reminding ourselves that glide cracks are to be avoided at all costs. They're incredibly unpredictable and when they fail, they often fail big as indicated in this g</span><a href="https://www.avalanche.ca/mountain-information-network/submissions/797ad42e-d019-40ab-9728-1a139f5ddde4" target="_blank"><span class="s_B5813F7D">reat MIN repor</span></a><span class="s_3FE45715">t.</span></p><p class="p_CC664AAA"><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/330f213d-8a1e-47f0-a27b-1d39216f7327" target="_blank"><span class="s_B5813F7D">This avalanche</span></a><span class="s_3FE45715"> was reported from the Duffey Lake area on Tuesday. It indicates the nature of the bond between the recent storm snow and old surfaces below may be poor. Most other recent reports from this region have been of small loose snow avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanches can be divided into two classes -- light triggers and large triggers. For light triggers there are reports of wind slabs up to size 2.5 on northerly aspects in northern areas . Throughout the region there were reports of a solar triggered cycle up to size 2 on solar aspects. Closer to Terrace there was a report of small soft slab triggered by a skier, a wind slab cycle up to size 1.5 (due to some strong southerly winds), and some loose dry avalanches, possibly as large as size 2. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Most recent avalanche activity was a result of larger triggers, namely explosives. Explosive tests and control resulted in mostly size 2 avalanches but some inland areas in the east side of the region avalanches up to size 3.5 were triggered.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Few observers in the field this week but reports are consistent with a natural avalanche cycle of storm and wind slabs up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3428770D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 15.3333333333333px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3428770D">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on all aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 30 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.</span><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several naturally triggered, size 1.5 storm slab avalanches and a few explosive triggered storm slabs up to size 2.5 were reported on primarily north aspects at treeline and above. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were reports of several human triggered avalanches up to size 2. A few of these were triggered remotely (from a distance). There were also several reports of natural storm slab avalanches up to size 3. These avalanches occurred on all aspects and at all elevation bands.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Widespread loose-dry avalanches were triggered by skiers on steep north-facing slopes as well as numerous wind slabs on alpine features on various aspects. They all remained small (size 1 to 1.5) and were confined to the recent snow near the surface. Sun has already affected the snow on steep south-facing slopes and triggered small loose wet avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few loose dry avalanches were noted in the Bow Valley today. In one observed case, the loosed dry triggered a slab mid slope. Probably a 2.5 all said and done.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity was reported on Wednesday. Explosive control produced small (size 1) slab avalanches on Tuesday. No other avalanches were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, two rider triggered persistent slab avalanches up to size 2 were reported on northerly aspects at treeline and below treeline. Additionally, a cornice failure triggered a size 2.5 persistent slab on a northeast facing treeline ridgetop.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on primarily solar aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 50 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, several rider triggered persistent slab avalanches up to size 2 were reported on a variety of aspects at treeline elevations. Human triggering of these persistent slabs is expected to increase with the forecast sunshine and warming.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, numerous naturally triggered wind slab avalanches up to size 2.5 and a few human triggered wind slabs up to size 1.5, were reported primarily on easterly aspects at treeline and above.</span><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
.s_94A968CE { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 14px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab after seeing many shooting cracks and whumpfs. See the </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_94A968CE">MIN</span></a><span class="s_A95EAA36"> report for more details. Several loose wet avalanches (size 1-1.5) were also triggered by riders on steep south facing slopes at treeline. A bit of natural activity, mainly loose avalanches, were observed on steep slopes. With this upcoming warming, natural avalanches are increasingly likely as the sun impacts solar aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
.s_36F41F30 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Two notable large natural persistent slabs releases were observed on northwest slopes at treeline on Thursday. A few natural avalanches (up to size 1.5), mainly dry-loose and thin wind slabs were also observed on steep slopes. Ridders were surprised to remotely trigger a small persistent slab avalanche down 60 cm late Thursday afternoon on a west facing slope below treeline. See the </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_36F41F30">MIN</span></a><span class="s_A95EAA36"> report from Lizard Range and Flathead for more details. With the upcoming warming natural avalanches are increasingly likely as the sun impacts solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanches can be divided into two classes -- light triggers and large triggers. For light triggers there are reports of wind and storm slabs up to size 2.5 on northerly aspects in northern areas . Throughout the region there were reports of a solar triggered cycle up to size 2 on solar aspects. Closer to Terrace there was a report of small soft slab triggered by a skier, a wind slab cycle up to size 1.5 (due to some strong southerly winds), and some loose dry avalanches, possibly as large as size 2. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Most recent avalanche activity was a result of larger triggers, namely explosives. Explosive tests and control resulted in mostly size 2 avalanches but in some inland areas in the east side of the region avalanches up to size 3.5 were triggered. Strong to extreme southwest wind Saturday combined with new storm snow is likely to initiate a natural avalanche cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There were few observers in the field this week but reports showed a natural avalanche cycle of storm and wind slabs up to size 2 early in the week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3428770D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 15.3333333333333px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a rider triggered size 2.5 persistent slab avalanche was reported on a west aspect at 2000 m. Another rider triggered size 2 persistent slab avalanche was triggered from 50 m. away from the slope that avalanched. It was a southwest aspect at 2300 m. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_3428770D">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on all aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 30 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.</span><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a few size 1 rider triggered persistent slab avalanches were reported on northerly aspects at treeline and below.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several naturally triggered, size 1.5 persistent slab avalanches and a few explosive triggered persistent slabs up to size 2.5 were reported on primarily north aspects at treeline and above. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were reports of several human triggered persistent slab avalanches up to size 2. A few of these were triggered remotely (from a distance). There were also several reports of natural persistent slab avalanches up to size 3. These avalanches occurred on all aspects and at all elevation bands.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">Numerous small (up to size 1.5) wind slabs were triggered by skiers on Thursday on various lee aspects at treeline and above. The sun has already affected the snow on steep south-facing slopes and triggered small loose wet avalanches at lower elevations. Natural and human triggered loose wet avalanches are likely with tomorrow's strong sun and steadily rising freezing level.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose dry avalanches up to sz 1.5 were observed on Friday.  Field teams were in before the temperatures really warmed up so there also may have been a few loose wet on steep solar aspects later in the day.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity was reported on Wednesday. Explosive control produced small (size 1) slab avalanches on Tuesday. No other avalanches were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, numerous natural loose wet and persistent slab avalanches up to size 2 were reported on solar aspects at all elevations. A skier triggered, persistent slab, size 2 avalanche was reported on a south aspect at 2000 m. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, two rider triggered persistent slab avalanches up to size 2 were reported on northerly aspects at treeline and below treeline. Additionally, a cornice failure triggered a size 2.5 persistent slab on a northeast facing treeline ridgetop.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on primarily solar aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 50 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, a natural size 2.5 and explosive triggered size 3 persistent slab avalanches were reported on north aspects in the alpine. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, several rider triggered persistent slab avalanches up to size 2 were reported on a variety of aspects at treeline elevations.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, numerous naturally triggered wind slab avalanches up to size 2.5 and a few human triggered wind slabs up to size 1.5, were reported primarily on easterly aspects at treeline and above.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
.s_36F41F30 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_A95EAA36">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_36F41F30">See the MIN report for more details</span></a><span class="s_A95EAA36">. I view this as an important piece of data when considering the effect of forecast strong sunshine and warming.</span></p><p class="p_CC664AAA"><span class="s_A95EAA36">Friday's reports were of wet loose avalanches to size 2 and skier triggered wind slabs to size 1.5 which is consistent with previous days trend. Explosives work was targetted on cornices and results were generally size 2 without any surprising results. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Small dry loose, wet loose, and small windslabs up to size 2 continue to be observed in the region.</span></p><p class="p_CC664AAA"><span class="s_DDF6C5E8">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_DDF6C5E8">See the MIN report for more details</span></a><span class="s_DDF6C5E8">. Although this occured in the neighbouring Lizard &amp; Flathead region, I view it as an important piece of data when considering the effect of forecast strong sunshine and warming.</span><span class="s_DDF6C5E8" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">I'll continue to divide recent avalanches into two classes -- light triggers and large triggers. For light triggers there are reports of wind slabs, storm slabs, and loose avalanches up to size 2.5; however, for me the most important avalanche data is SEVERAL REMOTELY TRIGGERED AVALANCHES (some of these reports were from areas outside the forecast region but are relevant to the region's conditions). Skiers are whumpfing the snowpack, often when they group up, wiith avalanches releasing at a distance (sometimes on the slope above). Reports include this happening on previously skied terrain, include releasing several avalanches from a single whumpf, and avalanches releasing and running over normal &quot;ski lines&quot;.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Explosives are the large triggers. Continued explosive tests and explosive control released up to size 3 avalanches from big terrain in a deep snowpack area by targetting cornices.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There are few observers in the field this week but reports showed a natural avalanche cycle of storm and wind slabs up to size 2 early in the week and loose wet avalanches with afternoon warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, several persistent slab avalanches up to size 2.5 were reported on a variety of aspects at treeline and above. The avalanches were failing on facets below the recent storm snow. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a rider triggered size 2.5 persistent slab avalanche was reported on a west aspect at 2000 m. Another size 2, persistent slab avalanche on a southwest aspect at 2300 m. was triggered by a skier from 50 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations. </span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on all aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 30 m. away from the slope that avalanched. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, two naturally triggered, size 2-2.5, persistent slab avalanches were reported on solar aspects in the alpine. Another persistent slab, size 2 avalanche was remotely triggered by a skier from 5 m. away on a southeast aspect at 2300 m. in steep, rocky terrain. Human triggering of these persistent slabs is expected to increase with the forecast sunshine and warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A couple of small wind and storm slabs were reported yesterday on northeast, east and south facing slopes. These avalanches were failing on the facet/crust combo just under the most recent snow, this activity is expected to pick up on Sunday and Monday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was observed observed over the past 24hrs except for isolated loose dry slides from steep unskiable terrain.  Clouds kept the temperature cool and loose wet slides were not a major issue. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from the last few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, numerous naturally triggered, persistent slab avalanches were reported on all aspects at treeline and above. Additionally, a snowcat triggered a size 1.5 avalanche on a steep road bank which reportedly failed on the surface hoar layer buried in mid-January. This is notable because it may indicate that this weak layer that has been dormant for many weeks is being brought back to life by the rapid warming of the snowpack.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, numerous natural loose wet and persistent slab avalanches up to size 2 were reported on solar aspects at all elevations. A skier triggered, persistent slab, size 2 avalanche was reported on a south aspect at 2000 m. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, several naturally triggered, persistent slab avalanches up to size 3 were reported on a variety of aspects in the alpine. Natural avalanche activity and size of avalanches are expected to increase during the next few days.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, a natural size 2.5 and explosive triggered size 3 persistent slab avalanches were reported on north aspects in the alpine. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_36F41F30 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #0000FF;text-decoration: underline; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_36F41F30">See the MIN report for more details</span></a><span class="s_A95EAA36">. I</span><span class="s_3FE45715"> view this as an important piece of data when considering the effect of forecast strong sunshine and warming.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Saturday's reports are of significant warming but only small loose wet avalanches. Neighbouring regions (for example Kananaskis Country) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers. IMHO this foretells the story of what's soon coming to a mountain range near you! </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_B5813F7D">See the MIN report for details</span></a><span class="s_3FE45715">. I view this as an important piece of data when considering the effect of forecast strong sunshine and warming.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Saturday's reports are of significant warming but only small loose wet avalanches. Neighbouring regions (for example Kananaskis Country) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers. IMHO this foretells the story of what's soon coming to a mountain range near you! </span><span class="s_DDF6C5E8" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday a few large avalanches were reported on solar aspects up the Railroad/Hurley Pass. On Saturday natural avalanches to size 2 were reported from solar aspects and several north aspects produced natural avalanches to size 1.5. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">As we enter a period of increased warming it's worth reminding ourselves that glide cracks are to be avoided at all times. They're incredibly unpredictable and when they fail, they often fail big. Glide avalanche concerns are especially important to consider in the Coquihalla area. A recent social media post from a professional in this part of the region does a great job of highlighting the issue. (</span><a href="https://www.facebook.com/groups/southcoasttouring/permalink/2319472218104449/" target="_blank"><span class="s_B5813F7D">Link here</span></a><span class="s_3FE45715">) A glide failed naturally on a southeast facing slope around 1000 m on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday a skier triggered a small wind slab at treeline that resulted in a broken leg. A few small wind slabs were observed on north facing alpine terrain and some natural cornice failure is beginning to be be observed too.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Fewer avalanche activity reports on Saturday and Sunday with smallish loose wet, loose dry, and windslabs.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">For me the most important avalanche data over the past few days were SEVERAL REMOTELY TRIGGERED AVALANCHES (some of these reports were from areas outside the forecast region but are relevant to the region's conditions). Skiers are whumpfing the snowpack, often when they group up, with avalanches releasing at a distance (sometimes on the slope above). Reports include this happening on previously skied terrain, include releasing several avalanches from a single whumpf, and avalanches releasing and running over normal &quot;ski lines&quot;.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There are few observers in the field this week but reports showed a natural avalanche cycle of storm and wind slabs up to size 2 early in the week and loose wet avalanches with afternoon warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, numerous naturally triggered, persistent slab avalanches up to size 3 were reported on all aspects/elevations. Natural avalanche activity and size of avalanches are expected to increase during the next few days.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, several persistent slab avalanches up to size 2.5 were reported on a variety of aspects at treeline and above. The avalanches were failing on facets below the recent storm snow. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a rider triggered size 2.5 persistent slab avalanche was reported on a west aspect at 2000 m. Another size 2, persistent slab avalanche on a southwest aspect at 2300 m. was triggered by a skier from 50 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations. </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, small cornice failures triggered small (size 1.5) slab avalanches on the slopes below. Cornice failures are expected to trigger large avalanches during the next few days.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, two naturally triggered, size 2-2.5, persistent slab avalanches were reported on solar aspects in the alpine. Another persistent slab, size 2 avalanche was remotely triggered by a skier from 5 m. away on a southeast aspect at 2300 m. in steep, rocky terrain. Human triggering of these persistent slabs is expected to increase with the forecast sunshine and warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Saturday (which was colder and cloudier than Sunday) initiated a natural avalanche cycle that featured loose moist avalanches to size 2.5 on south and southeast facing slopes between 1400 and 1600 m as the old storm snow slid on a crust before stepping down to basal (deep) weak layers.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday a couple of small wind and storm slabs were reported on northeast, east and south facing slopes. These avalanches were failing on the facet/crust combo just under the most recent snow, this activity likely picked up on Sunday and is expected to be even more active on Monday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was a widespread natural cycle (up to sz2.5) today. Solar aspects had loose wet avalanches at all elevations. The alpine &amp; treeline had windslabs and deeper slabs fail on all aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, a widespread loose wet avalanche cycle to size 3 and numerous size 3 persistent slabs were reported on solar aspects at all elevations. A natural avalanche cycle is expected to continue on all aspects and at all elevations on Tuesday.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, numerous naturally triggered, persistent slab avalanches were reported on all aspects at treeline and above. Additionally, a snowcat triggered a size 1.5 avalanche on a steep road bank which reportedly failed on the surface hoar layer buried in mid-January. This is notable because it may indicate that this weak layer that has been dormant for many weeks is being brought back to life by the rapid warming of the snowpack.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, a widespread loose wet avalanche cycle to size 2.5 and numerous size 3 persistent slabs were reported on solar aspects at all elevations. A natural avalanche cycle is expected to continue on all aspects and at all elevations on Tuesday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_36F41F30 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #0000FF;text-decoration: underline; } 
.s_A95EAA36 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday showed a continuation of natural loose wet avalanche activity focused on sun exposed aspects, with some releases reaching size 2.5 as they gouged into the snowpack to entrain more mass.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Saturday's reports are of significant warming but only small loose wet avalanches. Neighbouring regions (for example Kananaskis Country) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_36F41F30">See the MIN report for more details</span></a><span class="s_A95EAA36">. T</span><span class="s_3FE45715">his is an important piece of data when considering the effect of forecast strong sunshine and warming on persistent slab problems that developed earlier in the season.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, the type of activity shown above can be expected to continue, expand to all aspects, and perhaps intensify as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A report from Sunday in the Window Mountain area described snowshoeing party choosing to turn back after avoiding a large loose wet avalanche that ran into below treeline terrain. This highlights the importance of considering overhead hazards being warmed by the sun and potentially inverted (warmer at higher elevations) temperatures.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, a group of riders remotely triggered a size 1.5 persistent slab from 100 metres away. </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/1850960c-b13a-44df-ab94-c2014e9e3faf" target="_blank"><span class="s_B5813F7D">See the MIN report for details</span></a><span class="s_3FE45715">. I view this as an important piece of data when considering the effect of forecast strong sunshine and warming.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Saturday's reports showed initial warming producing only small loose wet avalanches. Neighbouring regions (for example Kananaskis Country) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers. Concern is increasing for deep basal snowpack weaknesses that have the potential to produce very large and destructive avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">With sunny skies and warming temperatures reports from region saw numerous natural loose wet avalanches from solar aspects up to size 2 in the alpine and at treeline. With continued warming we expect to see natural avalanche activity continue on all aspects and elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, numerous natural avalanches were reported up to size 2.5 in the Duffey Lake area and avalanches were reported on solar aspects up the Railroad/Hurley Pass. In the southern part of the region (Coquihalla) numerous loose wet avalanches were reported up to size 1.5 from solar aspects and widespread snowballing was seen on the northerly aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">As we enter a period of increased warming it's worth reminding ourselves that glide cracks are to be avoided at all times. They're incredibly unpredictable and when they fail, they often fail big. Glide avalanche concerns are especially important to consider in the Coquihalla area. A recent social media post from a professional in this part of the region does a great job of highlighting the issue. (</span><a href="https://www.facebook.com/groups/southcoasttouring/permalink/2319472218104449/" target="_blank"><span class="s_B5813F7D">Link here</span></a><span class="s_3FE45715">) A glide failed naturally on a southeast facing slope around 1000 m on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We suspect natural avalanche activity will persist with the sunny skies and warming temperatures throughout the forecast period. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from the Shames area on Sunday showed evidence of what was likely a widespread natural avalanche cycle that produced at least several very large (size 3) slab avalanches running the full extent of their respective avalanche paths. More numerous audible large avalanches were also reported. The failure plane in these slides appeared to have been our most recent storm snow interface. Even more numerous, smaller loose wet avalanches were observed. All of this activity was focused on steep, sun-exposed aspects. This type of activity can be expected to continue, potentially expand to all aspects, and intensify as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There are few observers in the field this week but reports showed a natural avalanche cycle of storm and wind slabs up to size 2 early in the week and loose wet avalanches with afternoon warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, a widespread loose wet avalanche cycle to size 3 and numerous size 3 persistent slabs were reported on solar aspects at all elevations. A natural avalanche cycle is expected to continue on all aspects and at all elevations on Tuesday. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, a widespread loose wet avalanche cycle to size 2.5 and numerous persistent slabs to size 3 were reported on solar aspects at all elevations. A natural avalanche cycle is expected to continue on all aspects and at all elevations on Tuesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, natural loose wet avalanches up to size 2 were reported from the region. These avalanches failed on all solar aspects (East through West) between 1600 to 2300 m. Saturday (which was colder and cloudier than Sunday) initiated a natural avalanche cycle that featured loose moist avalanches to size 2.5 on south and southeast facing slopes between 1400 and 1600 m as the old storm snow slid on a crust before stepping down to basal (deep) weak layers.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">With continued warming and a lack of overnight re-freeze we expect to see widespread natural avalanche activity on all aspects and elevations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">More avalanche activity again today, with slides up to size 2.5. Numerous loose wet avalanches occurred at all elevations. At Treeline and Alpine elevations wind slabs and deep persistent slabs were again active on all aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a widespread natural wet loose avalanche cycle occurred and was reported up to size 1.0. As the heat continues to penetrate the snowpack we suspect widespread natural wet avalanches will continue through the forecast period. These will be large and small avalanches on all aspects and elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle continued on Monday, producing small to large (size 1.5 to 3) avalanches on southeast to southwest aspects. The avalanches were at all elevations. There were also reports of slab avalanches around 30 to 40 cm deep, releasing on the interface described in the snowpack summary. They were on all aspects and between 1800 m and 2700 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed on Tuesday, from small to large (size 1 to 3). They occurred on southeast to southwest aspects and at all elevations. A wet slab avalanche was also observed on a south aspect with a depth of 60 cm, likely releasing on the weak layer described in the snowpack summary.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday and Monday showed a continuation of natural loose wet avalanche activity focused on sun exposed aspects, with some releases reaching size 2.5 as they gouged into the snowpack to entrain more mass. Several large persistent slab releases have also been noted failing on large alpine features and reaching size 2.5. Failure planes in these events remain uncertain, but at least one northeast aspect figured in these reports, showing some increasing potential for shaded aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Saturday's reports were of significant warming but only small loose wet avalanches. Neighbouring regions (for example Kananaskis Country) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, the type of activity shown above can be expected to continue, expand to all aspects, and perhaps intensify as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A report from Tuesday in the Elk Valley described numerous natural persistent slab releases reaching size 2 (large) on southeast aspects at around 2200 metres. Further to this activity, any sun-exposed snow became isothermal (slushy and lacking cohesion), and huge whumpfs that collapsed the basal snowpack were triggered during ski touring.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A report from Sunday in the Window Mountain area described snowshoeing party choosing to turn back after avoiding a large loose wet avalanche that ran into below treeline terrain. This highlights the importance of considering overhead hazards being warmed by the sun and potentially inverted (warmer at higher elevations) temperatures.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Given the above activity, loose wet avalanches remain a daily concern in steep, sun-exposed terrain (and in runout zones) while concern is increasing for deep basal snowpack weaknesses that have the potential to produce very large and destructive slab avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports indicated evidence of a natural loose wet avalanche cycle up to size 2 on Monday evening. Skier triggered loose wet avalanches were easily triggered up to size 1.5 and lots of snowballing and sluffing.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">With continued warming we expect to see natural avalanche activity to continue on all aspects and elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a widespread natural loose wet avalanche cycle up to size 3 was reported in the Northern half of the region. These avalanches failed on solar aspects (East, South and West). In the South, numerous natural avalanches were reported up to size 1.  </span></p><p class="p_CC664AAA"><span class="s_3FE45715">As we enter a period of increased warming it's worth reminding ourselves that glide cracks are to be avoided at all times. They're incredibly unpredictable and when they fail, they often fail big. Glide avalanche concerns are especially important to consider in the Coquihalla area. A recent social media post from a professional in this part of the region does a great job of highlighting the issue. (</span><a href="https://www.facebook.com/groups/southcoasttouring/permalink/2319472218104449/" target="_blank"><span class="s_B5813F7D">Link here</span></a><span class="s_3FE45715">) A glide failed naturally on a southeast facing slope around 1000 m on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We suspect natural avalanche activity will continue with the sunny skies and warming temperatures throughout the forecast period. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations in the Skeena corridor and Shames area on Sunday through Tuesday have been showing evidence of the ongoing natural avalanche cycle affecting all aspects and elevations. Numerous natural loose wet avalanches continue to be observed, with some reaching size 3 (very large). Explosives control yielded slabs that initiated at the March 10 interface but gouged deeply into isothermal (slushy) and faceted (sugary) snow. Observations show the largest loose wet avalanches reaching the full extent of their respective avalanche paths.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Initial reports of the avalanche cycle came from the Shames area on Sunday, with several very large (size 3) slab avalanches observed running full path with more numerous audible large avalanches. This initial activity was focused on steep, sun-exposed aspects. Remotely (from a distance) triggered avalanches have figured prominently in reports leading up to and during the current avalanche cycle. The March 10 interface has been the primary failure plane in slab releases.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The heightened avalanche activity described above can be expected to continue while temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday included an observation of a size 3 (very large) persistent slab running full path and within 100 metres of the viewing platform at Twin Falls. This highlights the current elevated danger in lower elevation areas threatened by large overhead avalanche paths. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Please see the Northwest Coastal forecast's avalanche summary for a description of the natural avalanche cycle that is ongoing in this neighbouring region. With limited observations inland, it is advised to treat this activity as an indication of potential in our region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose wet avalanches have been widespread and reaching size 2 (large), but were confined mainly to solar aspects on Monday. Only small (size 1) loose wet avalanches have been observed on north aspects thus far.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect the current heightened avalanche activity to continue, potentially expand to all aspects, and intensify as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle continued on Monday, producing small to large (size 1 to 3) avalanches on southeast to southwest aspects. The avalanches were at all elevations. There were also reports of slab avalanches around 30 to 50 cm deep, releasing on the interface described in the snowpack summary.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed on Monday, from small to large (size 1 to 3). They occurred on southeast to southwest aspects and at all elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, natural loose wet avalanches up to size 2 were reported from the region. These avalanches failed on all solar aspects (East through West) between 1600 to 2300 m. Some larger wet slab avalanches up to size 3 were also reported and triggered by explosives on southeast to southwest aspects between 1900-2200 m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Continued warming and a lack of overnight re-freeze we expect to see natural avalanche activity to continue on all aspects and elevations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">More avalanche activity again today, with slides up to size 2.5. Numerous loose wet avalanches occurred at all elevations. At Treeline and Alpine elevations wind slabs and deep persistent slabs were again active on all aspects. A few slabs were also observed on Northern aspects as the heat begins to settle the snowpack in these areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a widespread natural wet loose avalanche cycle occurred and was reported up to size 1.0. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">As the heat continues to penetrate the snowpack we suspect natural wet avalanches will continue through the forecast period. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle continued on Tuesday, producing small to large (size 1.5 to 3) avalanches on southeast to southwest aspects. The avalanches were at all elevations. A few persistent slab avalanches were also triggered naturally and by skiers. They were on all aspects, between 1800 m and 2800 m, and generally 40 to 100 cm deep.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed on Wednesday, from small to large (size 1 to 3). They occurred on southeast to southwest aspects and at all elevations. Wet slab avalanches were also observed, likely releasing on the weak layer described in the snowpack summary.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Tuesday's reports show continued loose wet avalanches reaching size 2 on sun-exposed aspects. Several loose wet avalanches were observed triggering smaller slab releases, thereby increasing in size and destructive potential.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday and Monday showed a continuation of natural loose wet avalanche activity focused on sun exposed aspects, with some releases reaching size 2.5 as they gouged into the snowpack to entrain more mass. Several large persistent slab releases have also been noted failing on large alpine features and reaching size 2.5. Failure planes in these events seem to indicate faceted snow in the mid-snowpack. At least one northeast aspect figured in these reports, suggesting some increasing potential for shaded aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, neighbouring regions (for example Kananaskis Country and the South Rockies) where the snowpack is thinner and weaker entered a natural avalanche cycle involving most aspects, most elevations, and most snowpack layers.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, the type of activity shown above can be expected to continue and potentially expand to all aspects as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A report from Tuesday in the Elk Valley described numerous natural persistent slab releases reaching size 2 (large) on southeast aspects at around 2200 metres. Further to this activity, any sun-exposed snow became isothermal (slushy and cohesionless), and huge whumpfs that collapsed the basal snowpack were triggered during ski touring.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A report from Sunday in the Window Mountain area described snowshoeing party choosing to turn back after avoiding a large loose wet avalanche that ran into below treeline terrain. This highlights the importance of considering overhead hazards being warmed by the sun and potentially inverted (warmer at higher elevations) temperatures.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Given the above activity, loose wet avalanches remain a daily concern in steep, sun-exposed terrain (and in runout zones) while concern is increasing for deep basal snowpack weaknesses that have the potential to produce very large and destructive slab avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, several natural and skier triggered loose wet avalanches up to size 2 were reported on all aspects and elevations from the region. Active cornice control with the use of explosives successfully dropped some chunks up to size 2 without pulling slabs on the slopes below. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanche activity may start to taper off with cooler temperatures this weekend. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, a few natural loose wet avalanches were reported from steep solar slopes. <br />On Tuesday, a natural loose wet avalanche cycle continued on sunny aspects (SE-W) up to size 3, some of these triggered thin slabs. On shady aspects (NW-NE) some slabs up to size 2 ran naturally. The crowns were 30-40 cm deep and we suspect they ran on a facet layer that developed during the cold spell in February.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">With continued warming it's worth reminding ourselves that glide cracks are to be avoided at all times. They're incredibly unpredictable and when they fail, they often fail big. Glide avalanche concerns are especially important to consider in the Coquihalla area. A recent social media post from a professional in this part of the region does a great job of highlighting the issue. (</span><a href="https://www.facebook.com/groups/southcoasttouring/permalink/2319472218104449/" target="_blank"><span class="s_B5813F7D">Link here</span></a><span class="s_3FE45715">) A glide failed naturally on a southeast facing slope around 1000 m on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We suspect that natural avalanche activity will slowly decrease as temperatures drop over the weekend. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations in the Skeena corridor and Shames area on Sunday through Tuesday have been showing evidence of the ongoing natural avalanche cycle affecting all aspects and elevations. Numerous natural loose wet avalanches continue to be observed, with some reaching size 3 (very large). Explosives control yielded slabs that initiated at the March 10 interface but gouged deeply into isothermal (slushy) and faceted (sugary) snow. Observations show the largest loose wet avalanches reaching the full extent of their respective avalanche paths.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Initial reports of the avalanche cycle came from the Shames area on Sunday, with several very large (size 3) slab avalanches observed running full path with more numerous audible large avalanches. This initial activity was focused on steep, sun-exposed aspects. The March 10 interface has been the primary failure plane in slab releases.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity has been similar if not more pronounced in the Bear Pass area and further north.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Expect the heightened avalanche activity described above to continue while temperatures remain elevated and overnight cooling weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday included an observation of a size 3 (very large) persistent slab running full path and within 100 metres of the viewing platform at Twin Falls. This highlights the current elevated danger in lower elevation areas threatened by large overhead avalanche paths. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Please see the Northwest Coastal forecast's avalanche summary for a description of the natural avalanche cycle that is ongoing in this neighbouring region. With limited observations inland, it is advised to treat this activity as an indication of potential in our region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose wet avalanches have been widespread and reaching size 2 (large), but were confined mainly to solar aspects on Monday. Only small (size 1) loose wet avalanches have been observed on north aspects thus far.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect heightened avalanche activity to continue and potentially expand to all aspects as temperatures remain elevated and overnight cooling remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle continued on Tuesday, producing small to large (size 1 to 3) avalanches on southeast to southwest aspects.  The avalanches were at all elevations. There were also a large slab avalanche that released on a south aspect at 2400 m, possibly releasing on the weak layer described in the snowpack summary.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed on Tuesday. They were large (up to size 2.5), occurred on southeast to southwest aspects, and at all elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a widespread natural loose wet and wet slab avalanche cycle occurred up to size 2.5. These avalanches were from sunny aspects (SE-SW) 1700-2000 m. Explosive controlled wet slab avalanches up to size 3 were also triggered on sunny aspects between 1900-2200 m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Continued warming and a lack of overnight re-freeze we expect to see natural avalanche activity to continue.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lots of loose wet avalanches in the PM. Any aspect that gets the sun has become reactive by mid day. Of note, many point release avalanches are triggering slabs as they flow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose wet avalanches up to size 1 were reported on Tuesday in the North Shore Mountains. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural activity may start to taper off with cooler temperatures this weekend. Until then you can expect loose wet slides to continue. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Wednesday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. A few slab avalanches were also triggered naturally, by skiers, and large machines. They occurred on all aspects and generally at treeline and alpine terrain. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle may continue on Friday on sun-exposed slopes, as temperatures remain exceptionally warm and the sun shines strong. The cycle should end on Saturday, as freezing levels drop and cloudy skies prevail.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Wednesday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. A notable persistent deep slab avalanche was also triggered on Wednesday, likely from a cornice fall. It was 100 cm deep on a northeast aspect at 2900 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle is expected to continue on Friday, as temperatures remain exceptionally warm and the sun shines strong. The cycle may end on Saturday, as freezing levels drop and cloudy skies prevail.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Wednesday's reports show continued loose wet avalanches reaching size 2 on sun-exposed aspects. Several avalanches that began as loose wet point releases, then triggered small slabs which entrained or gouged out additional mass, significantly increasing the size and destructive potential of the avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Reports from Sunday and Monday showed a continuation of natural loose wet avalanche activity focused on sun exposed aspects, with some releases reaching size 2.5 as they gouged into the snowpack to entrain more mass. Several large persistent slab releases have also been noted failing on large alpine features and reaching size 2.5. Failure planes in these events seem to indicate faceted snow in the mid-snowpack. At least one northeast aspect was included in these reports, suggesting some increasing potential for shaded aspects.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity is expected to continue until things cool off a bit.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, an explosive control mission produced an avalanche with every shot placed (nearly 20 in total). They were loose wet avalanches on sun-exposed slopes and dry, slab avalanches on northerly aspects, up to size 2.5. Additionally, large (size 2-2.5) loose wet natural avalanches continue to occur on solar aspects.</span></p><p class="p_CC664AAA"><span class="s_1681A555">A report from our South Rockies Field Team on Tuesday in the Elk Valley described numerous natural persistent slab releases reaching size 2 (large) on southeast aspects at around 2200 metres. Further to this activity, any sun-exposed snow became isothermal (slushy and cohesionless), and huge whumpfs that collapsed the basal snowpack were triggered during ski touring. Check out their video </span><a href="https://www.instagram.com/p/BvNeD2Jl99Q/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><a href="https://www.instagram.com/p/BvNeD2Jl99Q/" target="_blank" /><span class="s_1681A555">Given the above activity, loose wet avalanches remain a daily concern in steep, sun-exposed terrain (and in runout zones) while concern is increasing for deep basal (bottom of the snowpack) weaknesses that have the potential to produce very large and destructive slab avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, several loose wet avalanches up to size 1 were reported from steep solar terrain at lower elevations. Explosive control produced a size 2.5 loose wet avalanche on a southwest aspect between 1750-2050 m. It ended up triggering three slabs that failed at the ground. <br />On Wednesday, several natural loose wet avalanches up to size 2 released from sunny aspects. Skier controlled loose wet avalanches were also easily triggered up to size 2. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanche activity may start to slowly taper off with cooler temperatures this weekend. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural loose wet avalanche activity continued up to size 3 on SE-SW aspects in the northern parts of the region. In the South, a few natural loose wet avalanches were reported up to size 2 from steep solar aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">We suspect that natural avalanche activity will slowly decrease as temperatures drop over the weekend.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations in the Skeena corridor and Shames area on Sunday through Wednesday have been showing evidence of the ongoing natural avalanche cycle affecting all aspects and elevations. Numerous natural loose wet avalanches continue to be observed, with some reaching size 3 (very large). Explosives control yielded slabs that initiated at the March 10 interface but gouged deeply into isothermal (slushy) and faceted (sugary) snow. Observations show the largest loose wet avalanches reaching the full extent of their respective avalanche paths.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Initial reports of the avalanche cycle came from the Shames area on Sunday, with several very large (size 3) slab avalanches observed running full path with more numerous audible large avalanches. This initial activity was focused on steep, sun-exposed aspects. The March 10 interface has been the primary failure plane in slab releases.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity has been similar if not more pronounced in the Bear Pass area and further north.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Expect the heightened avalanche activity described above to continue while temperatures remain elevated and overnight cooling weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The natural avalanche activity has been slowing down a bit. However, as of Wednesday afternoon, naturally triggered loose wet avalanches up to 2.5 on sun-exposed aspects continue to be reported.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday included an observation of a size 3 (very large) persistent slab running full path and within 100 metres of the viewing platform at Twin Falls. This highlights the current elevated danger in lower elevation areas threatened by large overhead avalanche paths. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Please see the Northwest Coastal forecast's avalanche summary for a description of the natural avalanche cycle that is ongoing in this neighboring region. With limited observations inland, it is advised to treat this activity as an indication of potential similarities to this region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect heightened avalanche activity to continue and potentially expand to all aspects, so long as temperatures remain elevated and overnight freezing of the snow surface remains weak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Wednesday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. A couple persistent slab avalanches were also triggered by skiers, 40 to 80 cm deep and on south and north aspects in alpine terrain. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle may continue on Friday on sun-exposed slopes, as temperatures remain exceptionally warm and the sun shines strong. The cycle should end on Saturday, as freezing levels drop and cloudy skies prevail.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Wednesday. They were large (up to size 3), occurred on southeast to southwest aspects, and at all elevations. A wet slab avalanche was also observed. It was triggered naturally from the warming on a south aspect at 2300 m. It scrubbed to ground, with a thickness of 100 to 150 cm. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">This avalanche cycle may continue on Friday on sun-exposed slopes, as temperatures remain exceptionally warm and the sun shines strong. The cycle should end on Saturday, as freezing levels drop and cloudy skies prevail.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural loose wet avalanches continue on solar aspects up to size 2.5 through the region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanche activity will likely taper off on the weekend when temperatures and freezing levels start to drop to seasonal norms. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Wednesday. Natural loose wet avalanches up to size 1 were reported on Tuesday in the North Shore Mountains. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural activity may start to taper off with cooler temperatures this weekend. Until then you can expect loose wet slides to continue. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Thursday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. Numerous persistent and wet slab avalanches were also triggered naturally, by skiers, and explosives on Thursday. They occurred on all aspects and generally at treeline and alpine elevations.  They were most often 30 to 50 cm deep, with some of them releasing on the weak layer described in the snowpack summary.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The wet avalanche cycle will diminish over the weekend as cooler and cloudier weather prevails.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Thursday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. Many of these avalanches scoured to basal weaknesses. A notable deep persistent slab avalanche released on Wednesday, likely triggered by a cornice fall. It was 100 cm deep on a northeast aspect at 2900 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The wet avalanche cycle will diminish over the weekend as cooler and cloudier weather prevails.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Thursdays reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team </span><a id='GoToAdded' href="http://Thursdays reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team HERE." target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several avalanches that began as loose wet point releases, then triggered small slabs which entrained or gouged out additional mass, significantly increasing the size and destructive potential of the avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Expect the hazard to remain elevated until the clouds arrive and the temperatures cool.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, several loose wet avalanches up to size 1 were reported from steep solar terrain at lower elevations. Explosive control produced a size 2.5 loose wet avalanche on a southwest aspect between 1750-2050 m. It ended up triggering three slabs that failed at the ground. Active cornice control using explosives also produced a size 3 cornice failure which did not pull a slab avalanche from the slope below.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanche activity may start to slowly taper off with cooler temperatures this weekend. Human triggered avalanches are possible especially at lower elevations on southerly aspects due to a lack of re-freeze.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, no new avalanches were reported from the region.</span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">On Wednesday, natural loose wet avalanche activity continued up to size 3 on SE-SW aspects in the northern parts of the region. In the South, a few natural loose wet avalanches were reported up to size 2 from steep solar aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">We suspect that natural avalanche activity will slowly decrease as temperatures drop over the weekend.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity will taper off with the cloudy skies and cooling temperatures. Concern remains for human triggering persistent slab avalanches on a layer of facets that are down 50-100 cm. Explosive control work on Thursday produced several large avalanches, up to size 3, on this layer and there continue to be reports of skiers experiencing whumphing (collapsing) of this weak layer in shallow or variable snowpack areas in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Natural avalanche activity will taper off with the cloudy skies and cooling temperatures. Concern remains for human triggering persistent slab avalanches on a layer of facets that are down 30-50 cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Thursday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. A few large slab avalanches were also triggered on all aspects, running to valley bottom. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The wet avalanche cycle will diminish over the weekend as cooler and cloudier weather prevails.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between Sunday and Thursday. They were large (up to size 3), occurred on southeast to southwest aspects, and at all elevations. A persistent slab avalanche was also observed. It was triggered by a skier on a northeast aspect at 2300 m. It released within the faceted and hard wind-affected layer described in the snowpack summary. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The wet avalanche cycle will diminish over the weekend as cooler and cloudier weather prevails.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose wet avalanche activity continued on Thursday up to size 1.5. Natural avalanche activity will likely taper off later in the weekend when temperatures and freezing levels start to drop.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet and wet slab avalanches up to sz 2 were common on Friday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Thursday. <br />Natural loose wet avalanches up to size 1 were reported on Tuesday in the North Shore Mountains. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural activity may start to taper off with cooler temperatures this weekend. </span><span class="s_E6FD2046"> </span><span class="s_3FE45715">Human triggered avalanches are possible especially at lower elevations from southerly aspects due to a lack of re-freeze.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday has likely diminished, as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with avalanches up to size 3 mostly on southeast to southwest aspects. Numerous persistent and wet slab avalanches were also triggered naturally, by skiers, and explosives on Thursday and Friday. They occurred on all aspects and generally at treeline and alpine elevations. They were most often 30 to 50 cm deep.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between last Sunday and Friday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. Many of these avalanches scoured to basal weaknesses. A notable deep persistent slab avalanche released on Wednesday, likely triggered by a cornice fall. It was 100 cm deep on a northeast aspect at 2900 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The wet avalanche cycle will likely diminish this weekend as cooler and cloudier weather prevails.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity will taper off with the cloudy skies and cooling temperatures. Concern remains for human triggering persistent slab avalanches; especially on northerly aspects in the alpine.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Thursdays reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team </span><a id='GoToAdded' href="http://Thursdays reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team HERE." target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several avalanches that began as loose wet point releases, then triggered small slabs which entrained or gouged out additional mass, significantly increasing the size and destructive potential of the avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity will taper off with the cloudy skies and cooling temperatures. Concern remains for human triggering deep persistent slab avalanches; especially in rocky alpine terrain with a shallow or highly variable depth snowpack.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, there were numerous reports of skiers triggering what started as small loose wet avalanches and then gathered mass and entrained the entire snowpack to the ground running much further than expected, up to size 2. Check out this video from our South Rockies Field Team </span><a href="https://www.instagram.com/p/BvSiIzCFTDZ/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">A report from our South Rockies Field Team on Tuesday in the Elk Valley described numerous natural persistent slab releases reaching size 2 (large) on southeast aspects at around 2200 m. Further to this activity, any sun-exposed snow became isothermal (slushy and cohesionless), and large whumpfs that collapsed the basal snowpack were triggered during ski touring. Check out their video </span><a href="https://www.instagram.com/p/BvNeD2Jl99Q/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region on Friday loose wet avalanche activity to size 3 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. Very little activity was reported from areas closer to Whistler.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, several loose wet avalanches up to size 1 were reported from steep solar terrain at lower elevations. Explosive control produced a size 2.5 loose wet avalanche on a southwest aspect between 1750-2050 m. It ended up triggering three slabs that failed at the ground. Active cornice control using explosives also produced a size 3 cornice failure which did not pull a slab avalanche from the slope below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday loose wet avalanche activity up to size 3 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. No new activity was reported from the central or southern portions of the region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural loose wet avalanche activity continued up to size 3 on SE-SW aspects in the northern parts of the region. In the South, a few natural loose wet avalanches were reported up to size 2 from steep solar aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity has tapered off with the cloudy skies and cooling temperatures. Concern remains for human triggering persistent slab avalanches on a layer of facets that are down 50-100 cm. Explosive control work on Thursday produced several large avalanches, up to size 3, on this layer and there continue to be reports of skiers experiencing whumphing (collapsing) of this weak layer in shallow or variable snowpack areas in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Natural avalanche activity has tapered off with the cloudy skies and cooling temperatures. Concern remains for human triggering persistent slab avalanches on a layer of facets that are down 30-50 cm; especially in steep, rocky alpine terrain with a shallow or highly variable snowpack depth.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday has likely diminished, as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with avalanches up to size 3 mostly on southeast to southwest aspects. A few large slab avalanches were also triggered on all aspects, with many of them running to valley bottom.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday has likely ended, as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with avalanches up to size 3 mostly on southeast to southwest aspects. A persistent slab avalanche was also observed during the hot weather on Thursday. It was triggered by a skier on a northeast aspect at 2300 m. It released within the faceted and hard wind-affected layer described in the snowpack summary. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday natural loose wet activity to size 2 was reported throughout the region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Thursday or Friday. Natural activity will likely taper off with cooler temperatures Sunday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. Numerous persistent and wet slab avalanches were also triggered naturally, by skiers, and explosives on Thursday and Friday. They occurred on all aspects and generally at treeline and alpine elevations. They were most often 30 to 50 cm deep.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, avalanche problems will be split between lingering loose wet problems (areas of isothermal snow that haven't already avalanched) and isolated persistent slab problems on high north aspects. The latter may present as a large old wind slab that remains triggerable because it sits on an interface of preserved cold, faceted (sugary) snow. Small new wind slabs are expected to form gradually as new snow accumulates at higher elevations.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between last Sunday and Friday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. Many of these avalanches scoured to basal weaknesses. A notable deep persistent slab avalanche released on Wednesday, likely triggered by a cornice fall. It was 100 cm deep on a northeast aspect at 2900 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. The below link shows a smaller example of this sort of avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Thursdays reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team </span><a href="https://www.instagram.com/p/BvSiIzCFTDZ/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several avalanches that began as loose wet point releases, then triggered small slabs which entrained or gouged out additional mass, significantly increasing the size and destructive potential of the avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity has tapered off, but concern remains for human triggering deep persistent slab avalanches; especially in rocky alpine terrain with a shallow or highly variable depth snowpack.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, there were numerous reports of skiers triggering what started as small loose wet avalanches and then gathered mass and entrained the entire snowpack to the ground running much further than expected, up to size 2. Check out this video from our South Rockies Field Team </span><a href="https://www.instagram.com/p/BvSiIzCFTDZ/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">A report from our South Rockies Field Team on Tuesday in the Elk Valley described numerous natural persistent slab releases reaching size 2 (large) on southeast aspects at around 2200 m. Further to this activity, any sun-exposed snow became isothermal (slushy and cohesionless), and large whumpfs that collapsed the basal snowpack were triggered during ski touring. Check out their video </span><a href="https://www.instagram.com/p/BvNeD2Jl99Q/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday and Saturday loose wet avalanche activity to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. Very little activity was reported from areas closer to Whistler.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, several loose wet avalanches up to size 1 were reported from steep solar terrain at lower elevations. Explosive control produced a size 2.5 loose wet avalanche on a southwest aspect between 1750-2050 m. It ended up triggering three slabs that failed at the ground. Active cornice control using explosives also produced a size 3 cornice failure which did not pull a slab avalanche from the slope below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday and Saturday loose wet avalanche activity up to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. No new activity was reported from the central or southern portions of the region.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity has tapered off but concern remains for human triggering persistent slab avalanches on a layer of facets that are down 50-100 cm. Explosive control work on Thursday produced several large avalanches, up to size 3, on this layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Natural avalanche activity has tapered off, but concern remains for human triggering persistent slab avalanches on a layer of facets that are down 30-50 cm; especially in steep, rocky alpine terrain with a shallow or highly variable snowpack depth.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. A few large slab avalanches were also triggered on other aspects, with many of them running to valley bottom.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, avalanche problems will be split between lingering loose wet problems (areas of isothermal snow that haven't already avalanched) and isolated persistent slab problems on high north aspects. The latter may present as a large old wind slab that remains triggerable because it sits on an interface of preserved cold, faceted (sugary) snow. Small new wind slabs are expected to form gradually as new snow accumulates at higher elevations.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with avalanches up to size 3 mostly on southeast to southwest aspects. A persistent slab avalanche was also observed during the hot weather on Thursday. It was triggered by a skier on a northeast aspect at 2300 m. It released within the faceted and hard wind-affected layer described in the snowpack summary. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, avalanche problems will be split between lingering loose wet problems (areas of isothermal snow that haven't already avalanched) and isolated persistent slab problems on high north aspects. The latter may present as a large old wind slab that remains triggerable because it sits on an interface of preserved cold, faceted (sugary) snow. Small new wind slabs are expected to form gradually as new snow accumulates at higher elevations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from Saturday. On Friday natural loose wet activity to size 2 was reported throughout the region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. The lack of avalanche observations is probably linked to a slight cooling trend and the fact that the riding quality is poor in most locations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. A mix of persistent and wet slab avalanches were also triggered naturally, by skiers, and explosives on Thursday and Friday. These occurred on all aspects and generally at treeline and alpine elevations. They were most often 30 to 50 cm deep.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, cooling temperatures and inbound snowfall will shift concerns to new snow instabilities over the near term. These are likely to present initially as small new wind slabs forming on lee slopes at higher elevations. The re-emergence of the sun from Wednesday onward will shift us back into a spring pattern of loose wet avalanche concerns increasing with sun and warming each day.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many wet loose avalanches were observed between last Sunday and Friday. They were large (up to size 3), occurred mostly on southeast to southwest aspects, and at all elevations. Many of these avalanches scoured to basal weaknesses. A notable deep persistent slab avalanche released on Wednesday, likely triggered by a cornice fall. It was 100 cm deep on a northeast aspect at 2900 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, avalanche danger will remain linked with daytime warming and especially sun exposure. Light new snow amounts forecast for Tuesday will be the first to shed from steeper slopes as warming takes effect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. The below link shows a smaller example of this sort of avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Last Thursday reports show continued skier triggered loose wet avalanches reaching size 1.5 on sun-exposed aspects. Check out this video of our South Rockies Field Team </span><a href="https://www.instagram.com/p/BvSiIzCFTDZ/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555">Last Wednesday, several avalanches that began as loose wet point releases, then triggered small slabs which entrained or gouged out additional mass, significantly increasing the size and destructive potential of the avalanche.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity has tapered off, but concern remains for human triggering small loose wet avalanches that quickly gather mass and become dangerous. The link below is a small example of this concern.</span></p><p class="p_CC664AAA"><span class="s_1681A555">Last Thursday, there were numerous reports of skiers triggering what started as small loose wet avalanches and then gathered mass and entrained the entire snowpack to the ground running much further than expected, up to size 2. Check out this video from our South Rockies Field Team </span><a href="https://www.instagram.com/p/BvSiIzCFTDZ/" target="_blank"><span class="s_69909980">HERE.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No avalanche activity was reported on Sunday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday and Saturday loose wet avalanche activity to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. Very little activity was reported from areas closer to Whistler.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity has been reported. In the far north of the region on Friday and Saturday loose wet avalanche activity up to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">Natural avalanche activity has tapered off but concern remains for human triggering loose wet avalanches at lower elevations and&nbsp; persistent slab avalanches on northerly aspects in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Natural avalanche activity has tapered off, but concern remains for human triggering loose wet avalanches during the heat of the day and persistent slab avalanches in north facing alpine terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. A few large slab avalanches were also triggered on other aspects, with many of them running to valley bottom.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, cooling temperatures and inbound snowfall will shift concerns to new snow instabilities over the near term. These are likely to present initially as small new wind slabs forming on lee slopes at higher elevations. The re-emergence of the sun from Wednesday onward will shift us back into a spring pattern of loose wet avalanche concerns increasing with sun and warming each day.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The wet loose avalanche cycle from last Sunday to Friday diminished as cooler, seasonal temperatures returned to the mountains on Saturday. Evidence of the cycle is widespread at all elevations, with recent avalanches up to size 3 found mostly on southeast to southwest aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, cooling temperatures and inbound snowfall will shift concerns to new snow instabilities over the near term. These are likely to present initially as small new wind slabs forming on lee slopes at higher elevations. The re-emergence of the sun from Wednesday onward will shift us back into a spring pattern of loose wet avalanche concerns increasing with sun and warming each day. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from Saturday or Sunday. On Friday natural loose wet activity to size 2 was reported throughout the region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Preliminary reports from Tuesday in the Revelstoke area showed explosives control yielding mainly small (size 1-1.5) storm slab results, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Monday's reports showed</span><span class="s_E6FD2046"> </span><span class="s_3FE45715">some skier triggered small wind slabs composed of new snow at ridgetop as well as continued small natural loose wet avalanches at low elevations where the snowpack remains isothermal (slushy).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, new wind slabs should be the primary avalanche problem, but one that may become touchier with warming and possible sun exposure on Wednesday. The same sun and warming will reinvigorate loose wet avalanche problems over the coming days, with new snow being the first to shed from steeper slopes as warming takes effect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday showed included a few more 12-24 hour old observations of avalanches induced by recent warm temperatures. These included a size 2.5 glide slab at 2200 metres, a size 2 (large) loose wet avalanche at 1900 metres, and several small (size 1) wet slabs at 1250 metres. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, avalanche danger will remain linked with daytime warming and especially sun exposure. New snow from Tuesday's storm will be the first to shed from steeper slopes as warming takes effect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There are no reports of avalanche activity in the past few days.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday the expected solar input might trigger the new snow as loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday several loose avalanches and slab avalanches up to size 2 which released in the recent storm snow were reported. No avalanche activity was reported on Sunday and Monday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday and Saturday loose wet avalanche activity to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects. Very little activity was reported from areas closer to Whistler.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the far north of the region on Friday, Saturday, Monday and Tuesday loose wet avalanche activity up to size 2 was reported on solar aspects. Sporadic natural slab avalanches were also reported in the alpine and treeline, but no activity was reported from north aspects.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">A few glide slab avalanches up to size 2.5 have been reported near Terrace since Sunday on southerly slopes. Glide slabs typically happen on steep, smooth terrain features such as rock slabs or grassy slopes with little roughness. They are most common on southerly aspects, but during especially warm weather, may occur on shady aspects as well. Slopes with obvious large cracks (glide cracks) as well as slopes with a known history of glide releases are best avoided.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_DDF6C5E8 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14.6666666666667px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">When the sun comes out and temperatures rise during the day, loose wet avalanches will be very likely on sun-affected slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Preliminary reports from Tuesday in the Revelstoke area showed explosives control yielding mainly small (size 1-1.5) storm slab results, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Monday's reports showed some skier triggered small wind slabs composed of new snow at ridgetop as well as continued small natural loose wet avalanches at low elevations where the snowpack remains isothermal (slushy).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, new wind slabs should be the primary avalanche problem, but one that may become touchier with warming and possible sun exposure on Wednesday. The same sun and warming will reinvigorate loose wet avalanche problems over the coming days, with new snow being the first to shed from steeper slopes as warming takes effect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region, but neighbouring regions have shown some skier triggered small wind slabs composed of new snow at ridgetop as well as continued small natural loose wet avalanches at low elevations where the snowpack remains isothermal (slushy).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, new wind slabs should be the primary avalanche problem, but one that may become touchier with warming and possible sun exposure on Wednesday. The same sun and warming will reinvigorate loose wet avalanche problems over the coming days, with new snow being the first to shed from steeper slopes as warming takes effect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from Sunday or Monday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday showed skier traffic, ski cutting and explosives control yielding mainly small (size 1-1.5) storm slab releases, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, lingering wind slabs may remain reactive to human triggering and may become touchier with daytime warming. Meanwhile, an ample supply of new snow is in place to reinvigorate loose wet avalanche problems as sunshine and warming take hold each day.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in the Purcells on Tuesday, but reports from neighbouring regions showed new snow from Tuesday's storm reacting to skier traffic, ski cutting, and explosives control with 10-25 cm-deep slabs propagating easily and widely over previous surface crusts. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">All aspects were represented in reports, with a focus on north to northeast aspects as a result of loading by southwest winds. Similar conditions are likely to exist in areas of the Purcells that received more than a skiff of new snow from Tuesday's storm. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, lingering wind slabs (in areas with new snow) may still react to skier triggering and may also become touchier with warming. In some areas an ample supply of new snow is in place to reinvigorate loose wet avalanche problems as sunshine and warming take hold each day. Where less new snow exists, loose wet activity may be slightly more subdued.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There have been no reports of avalanches in the past few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday several loose avalanches and slab avalanches up to size 2 which released in the recent storm snow were reported. No avalanche activity was reported on Sunday and Monday.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region on Tuesday a natural size 2 loose wet avalanche and a skier triggered size 1 wind slab avalanche on a northerly aspect were reported. On Monday loose wet avalanche activity up to size 2 was reported on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A few glide slab avalanches up to size 2.5 have been reported near Terrace since Sunday on southerly slopes. Glide slabs typically happen on steep, smooth terrain features such as rock slabs or grassy slopes with little roughness. They are most common on southerly aspects, but during especially warm weather, may occur on shady aspects as well. Slopes with obvious large cracks (glide cracks) as well as slopes with a known history of glide releases are best avoided.</span><span class="s_1681A555" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday showed skier traffic, ski cutting, and explosives control yielding mainly small (size 1-1.5) storm slab releases, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the </span><span class="s_3FE45715">new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, lingering wind slabs may remain reactive to human triggering and may become touchier with daytime warming. Meanwhile, an ample supply of new snow is in place to reinvigorate loose wet avalanche problems as sunshine and warming take hold each day.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region, but reports from neighbouring regions showed new snow from Tuesday's storm reacting to skier traffic, ski cutting, and explosives control with 10-25 cm-deep slabs propagating easily over previous surface crusts. All aspects were represented in reports, with a focus on north to northeast aspects as a result of loading by southwest winds. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, lingering wind slabs may remain reactive to human triggering and may become touchier with daytime warming. Meanwhile, an ample supply of new snow is in place to reinvigorate loose wet avalanche problems as sunshine and warming take hold each day.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday and Wednesday there were reports of skier triggered thin wind slabs to size 1.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few loose dry avalanches on steep northern aspects were observed but no new slab avalanche activity. Observations were limited due to cloud cover and conditions. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Wednesday's reports showed similar activity to Tuesday, with more activity noted on all aspects with thicker wind-loaded slabs more prominent on north to east aspects and wet slabs and loose wet releases observed on sun-exposed south to west aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday showed skier traffic, ski cutting and explosives control yielding mainly small (size 1-1.5) storm slab releases, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in the Purcells over the past couple of days, but reports from </span><span class="s_3FE45715">neighbouring regions have shown the snow from Tuesday's storm reacting to skier traffic, ski cutting, and explosives control with 10-25 cm-deep slabs propagating easily over previous surface crusts. All aspects were represented in reports, with thicker wind-loaded slabs more prominent on north to east aspects and wet slabs observed on sun-exposed south to west aspects.</span><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Similar conditions were likely to exist in areas of the Purcells that received more than a skiff of new snow from Tuesday's storm. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There have been no reports of avalanches in the past few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday several loose dry and wind slab avalanches up to size 1.5 were observed on northerly aspects in the alpine and at treeline. A few wet loose avalanches up to size 2 were observed on solar aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday several loose avalanches and slab avalanches up to size were reported.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region on Wednesday several size 1 loose dry and wind slab avalanches were reported in the alpine and at treeline on north and west aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday a natural size 2 loose wet avalanche and a skier triggered size 1 wind slab avalanche on a northerly aspect were reported. On Monday loose wet avalanche activity up to size 2 was reported on solar aspects.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A few glide slab avalanches up to size 2.5 have been reported near Terrace since Sunday on southerly slopes. Glide slabs typically happen on steep, smooth terrain features such as rock slabs or grassy slopes with little roughness. They are most common on southerly aspects, but during especially warm weather, may occur on shady aspects as well. Slopes with obvious large cracks (glide cracks) as well as slopes with a known history of glide releases are best avoided.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Wednesday's reports showed similar activity to Tuesday, with more activity noted on all aspects </span><span class="s_3FE45715">with thicker wind-loaded slabs more prominent on north to east aspects and wet slabs and loose wet releases observed on sun-exposed south to west aspects.</span><span class="s_3FE45715" /></p><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday showed skier traffic, ski cutting, and explosives control yielding mainly small (size 1-1.5) storm slab releases, with slab depths of 10-20 cm. North to northeast aspects were the focal point and wide fracture propagations in these results were attributed to a poor bond between the new snow and the previous surface of crust.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Several natural loose wet and storm slab avalanches were reported in the region on Wednesday. Similar but more numerous reports from neighbouring regions have shown the snow from Tuesday's storm reacting to skier traffic, ski cutting, and explosives control with 10-25 cm-deep slabs propagating easily over previous surface crusts. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">All aspects were represented in reports, with thicker wind-loaded slabs more prominent on north to east aspects and wet slabs observed on sun-exposed south to west aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday and Wednesday there were reports of skier triggered thin wind slabs to size 1.5. On Wednesday loose wet avalanches to size 1 were observed in the afternoon on solar aspects.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous sluffs within the new storm snow were observed on solar aspects but the cloud cover kept the solar radiation to a minimum. Friday is to be sunnier, so more activity is expected.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, several size 1-1.5 wind slab avalanches were triggered in the alpine (15-30 cm thick). One natural size 1.5 persistent slab avalanche occurred on a southwest aspect at 2100 m with limited propagation.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Earlier in the week, wind slabs were reported on north and east aspects while loose wet releases were observed on sun-exposed south to west aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Minimal avalanche activity has been reported in the Purcells over the past couple days. One small naturally-triggered wind slab was observed on a northeast alpine slope on Thursday. Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there was a report near Fernie of a skier triggered, size 2.5 wet slab avalanche that began as a loose wet avalanche and then gathered mass which ran much further than expected through low angle terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, there were reports of a few loose wet avalanches up to size 1.5 out of steep, sun-exposed terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday several skier triggered up to size 1.5 wind slab avalanches at isolated terrain features as for example along ridges were reported.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Over the past couple of days several loose dry and wind slab avalanches up to size 1.5 were observed on northerly aspects in the alpine and at treeline. A few wet loose avalanches up to size 2 were also observed on solar aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday no new avalanche activity was observed.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region on Wednesday several size 1 loose dry and wind slab avalanches were reported in the alpine and at treeline on north and west aspects. On Tuesday a natural size 2 loose wet avalanche and a skier triggered size 1 wind slab avalanche on a northerly aspect were reported. On Monday loose wet avalanche activity up to size 2 was reported on solar aspects.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, loose wet avalanches (size 1-2) have been observed on sun-exposed south to west facing slopes and wind slabs (size 1-2) reported on north to east aspects. North to northeast aspects were the focal point for slab avalanches with wide fracture propagations attributed to a poor bond between the new snow and old crusts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Activity on Thursday was limited to a small skier triggered wind slab on a north-facing alpine slope. Several natural loose wet and storm slab avalanches were reported earlier in the week following Tuesday's storm.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday only few small loose wet and loose dry avalanches were observed. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday loose wet avalanches to size 1 were observed in the afternoon on solar aspects. On Tuesday and Wednesday there were reports of skier triggered thin wind slabs to size 1.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few new loose wet slides up to sz 1 were observed in steep solar terrain on Friday.  No new slab activity was noted. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches on south-facing slopes have been the predominant type of avalanche activity over the past few days. Small (size 1) wind slabs in the alpine have also been reactive to human triggering over the past week, but activity has dwindled recently.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, watch for loose wet avalanches if the sun pokes out, and remain cautious of wind slabs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Minimal avalanche activity has been reported in the Purcells over the past few days. A few small wind slabs have been reported on northeast alpine slopes and loose wet avalanches have been observed in steep south-facing terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, watch for loose wet avalanches if the sun pokes out, and remain cautious of wind slabs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, there were reports of a few loose wet avalanches up to size 1.5 out of steep, sun-exposed terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday there were reports of several skier triggered size 1.5 wind slab avalanches in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent reports of avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 2 loose wet and wet slab avalanches on southerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be likely on sun-affected slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday a few large (size 2-3) skier triggered slab avalanches were reported on north-facing slopes above 2300 m. This highlights the fact winter-like conditions can still be found in shaded alpine terrain, as several other size 1-2 slab avalanches have been reported in this type of terrain over the past few days. Elsewhere, the predominant avalanche activity has been loose wet avalanches on sun-exposed slopes (mostly south and west facing).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. Several loose wet and storm slab avalanches were reported earlier in the week following Tuesday's storm.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday a few loose wet and loose dry avalanches were observed to size 1. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Riders have triggered a few small (size 1) slabs in north-facing alpine terrain over the past few days (see this </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/a5fdc8a1-c7cf-4172-98cc-603cc236444a" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715"> for an example). Although small, they serve as a reminder to use caution above cliffs and terrain traps where small avalanches could have severe consequences. Small loose wet avalanches also remain possible on sun-exposed slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No notable avalanches have been reported over the past few days. Activity has been limited to a few small wind slabs on northeast alpine slopes and loose wet avalanches on sun-exposed slopes. Expect the same pattern to continue.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span><span class="s_3FE45715" /></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, there were reports of a few loose wet avalanches up to size 1.5 out of steep, sun-exposed terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The most recent avalanche activity was of a skier triggered size 1 wind slab avalanche on Saturday on a north aspect at the upper end of tree line.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be possible on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 2 loose wet and wet slab avalanches on southerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as the sun comes out and temperatures rise.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a few large (size 2-3) skier triggered slab avalanches were reported on north-facing slopes above 2300 m. Some other smaller slabs have been reported in the same type of terrain over the past few days, highlighting the fact winter-like conditions can still be found in shaded alpine terrain. Small loose wet avalanches remain possible on sun-exposed slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no new reports of recent avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new observed today (limited field observations), but recent loose wet avalanche activity up to size 1.5 has been occurring most days during the peak of the air temperatures and/or intense solar radiation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Riders have triggered a few small slabs (size 1) in north-facing alpine terrain over the past few days (see this </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/a5fdc8a1-c7cf-4172-98cc-603cc236444a" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715"> for an example). Although small, they serve as a reminder to use caution above cliffs and terrain traps where small avalanches could have severe consequences. Small loose wet avalanches also remain possible on sun-exposed slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No notable avalanches have been reported over the past few days. Activity has been limited to a few small wind slabs on northeast alpine slopes and loose wet avalanches on sun-exposed slopes. Expect the same pattern to continue.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Last Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Friday, there were reports of a few loose wet avalanches up to size 1.5 out of steep, sun-exposed terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent reports of avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">When the sun comes out and temperatures rise during the day, loose wet avalanches will be possible on sun-affected slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 2 loose wet and wet slab avalanches on southerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as the sun comes out and temperatures rise.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small wind slabs were reported in north alpine terrain over the weekend. On Friday, a few larger skier triggered slab avalanches (size 2-3) were reported on north-facing slopes above 2300 m. These avalanches highlight the fact winter-like conditions can still be found in shaded alpine terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, one size 2 wet slab avalanche was reported on an east aspect at 1800 m. Otherwise, no recent avalanches have been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no new reports of recent avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed on Monday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A couple storm slab avalanches were triggered by explosives on Monday, on north aspects around 2500 m. They were 50 cm deep. Otherwise, no new avalanches were observed.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Last Wednesday, there were reports of a few size 1 loose wet avalanches in the Fernie area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time or as temperatures rise, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Monday, small (small 1-1.5) loose-dry and loose-wet avalanches were reported with the accumulated snowfall as well as two small (size 1-1.5) storm slab avalanches triggered with explosives. On Tuesday, snowballing was observed in alpine terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent reports of avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Last Friday, there were reports of a few size 2 loose wet and wet slab avalanches on southerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as the sun comes out and temperatures rise. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as the sun comes out and temperatures rise.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a small (size 1) wind slab was triggered by a skier on a north aspect in alpine terrain. The slab was 20 cm deep and about 10 m wide. Otherwise, no other avalanches were observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A cornice fall was observed on Monday, which did not trigger a slab on the slope below. Otherwise, no other avalanches were observed.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no new reports of recent avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wet slides either in the form of slabs or loose are occuring daily with the temperature increases.  In general we are seeing slides mainly in the sz 2 range but large avalanches are possible due to the deeper weak layers.  Always be thinking about consequence as you travel.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there was a report of one size 2 natural loose wet avalanche on a south aspect at 2400 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of natural slab avalanches, size 2-2.5. The size 2 was a west aspect on a steep moraine feature at 2100 m. The size 2.5 was on a northeast aspect at 2300 m and was triggered by an ice fall on a glacier. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">A few storm slab avalanches were triggered by explosives on Monday, on north aspects around 2500 m. They were 50 cm deep. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There have been no recent avalanche observations in the forecast region.</span></p><p class="p_CC664AAA"><span class="s_1681A555">If the sun comes out for prolonged periods of time, the chances of loose avalanches will increase, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The chances of loose avalanches will increase as the sun comes out or as temperatures rise, especially in areas with fresh snow.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Monday, small (small 1-1.5) loose-dry and loose-wet avalanches were reported with the accumulated snowfall as well as two small (size 1-1.5) storm slab avalanches triggered with explosives. On Tuesday, snowballing was observed in steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent reports of avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Last Friday, there were reports of a few size 2 loose wet and wet slab avalanches on southerly aspects. The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as the sun comes out and temperatures rise. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent avalanche observations in the forecast region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of glide slab avalanches, size 1 and 2.5. These occurred on southeast aspects between 2200-2400 m. Both released on rock slabs.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a small (size 1) wind slab was triggered by a skier on a north aspect in alpine terrain. The slab was 20 cm deep and about 10 m wide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A cornice fall was observed on Tuesday, which triggered a small, thin slab avalanche on a steep, unsupported roll.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Another cornice fall was observed on Monday, but it did not trigger a slab on the slope below. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no new reports of recent avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. Expect to see an increase of storm snow activity with 20-40 cm of new snow at uppermost elevations within the region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there was a report of an explosives triggered size 1.5 slab avalanche.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there was a report of one size 2 natural loose wet avalanche on a south aspect at 2400 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of natural slab avalanches, size 2-2.5. The size 2 was a west aspect on a steep moraine feature at 2100 m. The size 2.5 was on a northeast aspect at 2300 m and was triggered by an ice fall on a glacier. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">A few storm slab avalanches were triggered by explosives on Monday, on north aspects around 2500 m. They were 50 cm deep. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There have been no recent avalanche observations in the forecast region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Monday, small (small 1-1.5) loose-dry and loose-wet avalanches were reported with the accumulated snowfall as well as two small (size 1-1.5) storm slab avalanches triggered with explosives. On Tuesday, snowballing was observed in steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small storm slab avalanches were triggered by skiers on Wednesday. They were 10 to 20 cm thick, above 1700 m, and on all aspects. The likelihood of triggering avalanches will increase above the snow-rain line due to continuous snowfall this weekend.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small storm slab avalanches were triggered by skiers and naturally on Wednesday. They were 10 cm thick and generally on northerly aspects. The likelihood of triggering avalanches will increase above the snow-rain line due to continuous snowfall this weekend.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent avalanche observations in the region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent avalanche observations in the forecast region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of glide slab avalanches, size 1 and 2.5. These occurred on southeast aspects between 2200-2400 m. Both released on rock slabs.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a small (size 1) wind slab was triggered by a skier on a north aspect in alpine terrain. The slab was 20 cm deep and about 10 m wide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There has been three cornice failures observed in the region since Monday (one per day).&nbsp; One triggered a large avalanche that scrubbed down to the base of the snowpack, one triggered a thin slab avalanche and one did not trigger a slab. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed on Wednesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region on Wednesday. The likelihood of triggering avalanches is increased at and above the snow-rain line due to the continuous snowfall.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reactive storm slabs may be found at upper elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few natural, human and explosives triggered storm slab avalanches up to size 1.5, as well as a few size 1 loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there was a report of one size 2 natural loose wet avalanche on a south aspect at 2400 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were a few reports of natural and human triggered storm and wind slab avalanches in the alpine, as well as a few human triggered loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of natural slab avalanches, size 2-2.5. The size 2 was a west aspect on a steep moraine feature at 2100 m. The size 2.5 was on a northeast aspect at 2300 m and was triggered by an ice fall on a glacier. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 1 were reported from steep alpine features on Thursday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity to report. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Many small avalanches were triggered by skiers and naturally on Thursday, within the recent storm snow. They ranged from slab to loose, occurred on all aspects, and generally at treeline and alpine terrain. The likelihood of triggering avalanches will increase above the snow-rain line due to more stormy conditions this weekend.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, small loose wet avalanches were triggered naturally and by skiers within the recent storm snow. The likelihood of triggering avalanches will increase above the snow-rain line due to stormy conditions this weekend.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent avalanche observations in the region. If you're out this weekend we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">There have been no recent avalanche observations in the region. If you're out this weekend we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reactive storm slabs may be found at upper elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were several reports of natural and human triggered storm slab avalanches up to size 1.5, as well as a few natural loose wet avalanches up to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of glide slab avalanches, size 1 and 2.5. These occurred on southeast aspects between 2200-2400 m. Both released on rock slabs.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">It is likely that storm slabs will be reactive to human triggering at upper elevations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few human triggered size 1 loose wet avalanches at treeline within the new snow.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There has been three cornice failures observed in the region since Monday. One triggered a large avalanche that scrubbed down to the base of the snowpack, one triggered a thin slab avalanche and one did not trigger a slab. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous wind slabs and loose wet avalanches were observed on Thursday. They were reactive to skiers, explosives, and loose wet avalanches occurred naturally during daytime warming. They were all within the recent storm snow.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. The likelihood of triggering avalanches is increased at and above the snow-rain line due to the stormy weather expected this weekend.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 1 human triggered storm slab avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few natural, human and explosives triggered storm slab avalanches up to size 1.5, as well as a few size 1 loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there was a report of one size 2 natural loose wet avalanche on a south aspect at 2400 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were a few reports of natural and human triggered storm and wind slab avalanches in the alpine, as well as a few human triggered loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 1 were reported from steep alpine features on Thursday. No significant avalanche activity to report from Friday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant avalanche activity to report from the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small storm slabs were triggered by skiers on Friday, within the recent storm snow up to 40 cm thick. The likelihood of triggering avalanches is increased above the snow-rain line due to stormy conditions this weekend and the potential for loose wet avalanches if the sun shines.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were observed in the region on Friday. The likelihood of triggering loose wet avalanches will increase on Sunday if the sun shines.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday loose wet avalanches to size 1 were reported as storm snow slid on the April 4th crust. A few natural size 1 to 1.5 wind slabs were reported Saturday morning. If you're out this weekend we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant recent avalanche activity to report. If you're out this weekend we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few natural and human triggered storm and wind slab avalanches up to size 2. These were mainly on north to east aspects in the alpine.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were several reports of natural and human triggered storm slab avalanches up to size 1.5, as well as a few natural loose wet avalanches up to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, there were two reports of glide slab avalanches, size 1 and 2.5. These occurred on southeast aspects between 2200-2400 m. Both released on rock slabs.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few human triggered size 1 loose wet avalanches at treeline within the new snow.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There has been three cornice failures observed in the region since Monday. One triggered a large avalanche that scrubbed down to the base of the snowpack, one triggered a thin slab avalanche and one did not trigger a slab. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small loose wet avalanches were observed on Friday during daytime warming. They released within the recent storm snow.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. The likelihood of triggering avalanches is increased above the snow-rain line due to stormy conditions this weekend and the potential for loose wet avalanches if the sun shines.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were reports of several natural, human and explosives triggered wind slab and storm slab avalanches up to size 1.5 at treeline and alpine elevations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 1 human triggered storm slab avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few natural, human and explosives triggered storm slab avalanches up to size 1.5, as well as a few size 1 loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were a few reports of natural and human triggered wind slab avalanches, mainly in the alpine on north and east facing slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were a few reports of natural and human triggered storm and wind slab avalanches in the alpine, as well as a few human triggered loose wet avalanches.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous loose avalanches to size 1.5 were reported from terrain that generally faces north around 2000 m on Saturday. A natural cornice failure also produced a size 2 slab on a northeast facing slope at 2200 m on Saturday.&nbsp; </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant avalanche activity to report from the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small (size 1-1.5) storm slabs and wind slabs were reactive to skier traffic. Cornices were reactive to explosives and triggered large (size 2) slab avalanches as they fell on the slopes below. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Small storm slabs were triggered by skiers on Friday, within the recent storm snow up to 40 cm thick. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small wind slab pockets were reactive to skiers in cross-loaded features at treeline near the Duffey.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase on if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday loose wet avalanches to size 1 were reported as storm snow slid on the April 4th crust. A few natural size 1 to 1.5 wind slabs were reported Saturday morning. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant recent avalanche activity to report. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were a few reports of natural and human triggered storm slab and wind slab avalanches up to size 1.5 at treeline and alpine elevations. There were also reports of human triggered loose wet avalanches below treeline.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few natural and human triggered storm and wind slab avalanches up to size 2. These were mainly on north to east aspects in the alpine.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were several reports of natural and human triggered storm slab avalanches up to size 1.5, as well as a few natural loose wet avalanches up to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there was a report of a human triggered size 1.5 wind slab avalanche on a northeast aspect at 2600 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were reports of a few human triggered size 1 loose wet avalanches at treeline within the new snow.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered small (size 1-1.5) storm slab avalanches up to 30 cm deep. Skier traffic triggered small pockets of storm snow with the deepest (up to 40 cm) and most reactive deposits in specific lee terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small loose wet avalanches were observed on Friday during daytime warming. Continuing with the spring theme, the likelihood of triggering loose wet avalanches will increase if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wet slides either in the form of slabs or loose are occurring most days when the temperature and solar radiation increases. In general we are seeing slides mainly in the size 1 to 2 range, but large avalanches are possible due to the deeper weak layers. Always be thinking about consequence as you travel. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of loose wet avalanches on sun-affected slopes will increase throughout the day as temperatures rise and the snowpack warms, especially in areas where fresh snow has accumulated.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there were reports of several natural and human triggered wet and dry loose avalanches up to size 1.5 at treeline and in the alpine on south aspects and slab avalanches up to size 2 in the alpine on north aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were reports of several natural, human and explosives triggered wind slab and storm slab avalanches up to size 1.5 at treeline and alpine elevations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few size 1 human triggered storm slab avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Small (size 1-1.5) wind slabs were reactive to skiers on Sunday, generally around ridgetops and steep, convex terrain above 2200 m. The most reactive deposits were in immediate lee features, including a size 2 wind slab avalanche remotely triggered from a rocky saddle 10 m away. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were a few reports of natural and human triggered wind slab avalanches, mainly in the alpine on north and east facing slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were a few reports of natural and human triggered storm and wind slab avalanches in the alpine, as well as a few human triggered loose wet avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday there was a natural loose wet avalanche cycle to size 1.5 on solar aspects as the new snow ran on the crust. On Sunday storm slabs to size 1.5 were susceptible to explosive control work to size 1.5 on north and northeast facing terrain between 1900 and 2000 m. Numerous loose avalanches to size 1.5 were reported from terrain that generally faces north around 2000 m on Saturday. A natural cornice failure also produced a size 2 slab on a northeast facing slope at 2200 m on Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region, the following is all from the neighboring Lizard Range and Flathead region: On Monday there was a natural loose wet avalanche cycle to size 1.5 on solar aspects as the new snow ran on the crust. On Sunday storm slabs to size 1.5 were susceptible to explosive control work to size 1.5 on north and northeast facing terrain between 1900 and 2000 m. Numerous loose avalanches to size 1.5 were reported from terrain that generally faces north around 2000 m on Saturday. A natural cornice failure also produced a size 2 slab on a northeast facing slope at 2200 m on Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche control work with explosives triggered mostly small storm slabs (size 1-1.5) and cornices in alpine and treeline on Sunday; these avalanches failed on the storm snow - melt-freeze crust interface.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small (size 1-1.5) storm slabs and wind slabs were reactive to skier traffic. Cornices were reactive to explosives and triggered large (size 2) slab avalanches as they fell on the slopes below. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Small storm slabs were triggered by skiers on Friday, within the recent storm snow up to 40 cm thick. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle to size 2 likely occurred overnight Saturday; slab avalanches to size 2 were observed on north-northeasterly aspects around ridgetops and in recently loaded lee features on Sunday. Explosives also triggered small (size 1-1.5) wind slab avalanches on north to west aspects about 2000 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small wind slab pockets were reactive to skiers in cross-loaded features at treeline near the Duffey.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase on if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">We received a great MIN report from the Shames backcountry that describes an active wet loose avalanche cycle to size 1.5, more details </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/52d2a82b-d285-4609-841c-a969297052de" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. Wind slab avalanches were susceptible to explosive triggering on Sunday to size 2.5 as well. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant recent avalanche activity to report. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, there were reports of a natural storm slab size 2.5 on an east aspect in the alpine and several natural dry and moist loose avalanches up to size 2.5 on northerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday and Saturday, there were a few reports of natural and human triggered storm slab and wind slab avalanches up to size 2 at treeline and alpine elevations. There were also reports of several natural and human triggered loose wet avalanches up to size 1.5 on steep solar slopes and below treeline.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there were reports of a few natural and human triggered storm and wind slab avalanches up to size 2. These were mainly on north to east aspects in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday wind slabs to size 2 released naturally and were also susceptible to human triggering on north, northeast and east facing terrain between 1900 and 2200 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there was a report of a human triggered size 1.5 wind slab avalanche on a northeast aspect at 2600 m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there were reports of numerous natural, human and explosive triggered storm slab avalanches up to size 2.5 at treeline and in the alpine on all aspects (see this </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/06ce6624-4ca5-45e8-916a-26744aed6d38" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715">).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered small (size 1-1.5) storm slab avalanches up to 30 cm deep. Skier traffic triggered small pockets of storm snow with the deepest (up to 40 cm) and most reactive deposits in specific lee terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small loose wet avalanches were observed on Friday during daytime warming.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wet slides either in the form of slabs or loose are occurring most days when the temperature and solar radiation increases. Cornice failures are also becoming more common. In general we are seeing slides mainly in the size 1 to 2 range, but large avalanches are possible due to the deeper weak layers. Always be thinking about consequence as you travel. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a size 2 human triggered slab avalanche on an east aspect in the alpine was reported as well as a size 1.5 explosive triggered cornice which didn't trigger an avalanche on the slope. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural and human triggered loose wet avalanches up to size 2 were observed on sun exposed slopes in the alpine. There were also reports of several natural, human and explosive triggered storm slab avalanches and wind slabs in immediate lee features up to size 2 in the alpine on west, north and east aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, there were a few reports of natural and human triggered wind slab avalanches, mainly in the alpine on north and east facing slopes.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, small (size 1-1.5) wind slabs were reactive to skiers, generally around ridge crests and steep, convex terrain above 2200 m. The most reactive deposits were in immediate lee features, including a size 2 wind slab avalanche remotely triggered from a rocky saddle 10 m away. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Overnight Sunday, a natural avalanche cycle to size 2 occurred on the western side of the Purcell Forecast region. Storm slab avalanches were observed on steep alpine slopes on all aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday no new avalanches were reported. On Monday there was a natural loose wet avalanche cycle to size 1.5 on solar aspects as the new snow ran on the crust. Snowfall amounts are uncertain for the next 24 hours. Storm slabs may only be an avalanche problem with new snow and loading.</span><span class="s_AA239A9B"><br /></span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight re-freeze and how quickly the snowpack is warmed up.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region, the following is all from the neighboring Lizard Range and Flathead region: </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">On Tuesday, numerous natural loose wet avalanches up to size 1.5 occurred mostly from sunny aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight re-freeze and how quickly the snowpack is warmed up.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, natural storm slab avalanches to size 2 were observed on north to northeast aspects around 2200-2400 m in the Whistler Backcountry, initiating from steep, lee start zones. 2 separate groups of skiers in the Whistler Backcountry triggered slab avalanches (size 1.5-2) on north-northeast aspects in the alpine, including this Decker Main MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, avalanche control work with explosives triggered mostly small storm slabs (size 1-1.5) and cornices in alpine and treeline; these avalanches failed on the storm snow - melt-freeze crust interface.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small (size 1-1.5) storm slabs and wind slabs were reactive to skier traffic. Cornices were reactive to explosives and triggered large (size 2) slab avalanches as they fell on the slopes below. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from the Whistler Backcountry </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a skier triggered slab avalanche on a north-northeast alpine aspect on Monday. The avalanche was triggered in lee-ward terrain below a ridge feature. While outside the forecast region, the avalanche highlights a similar terrain feature that may hold wind slabs in the South Coast Inland.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle to size 2 likely occurred overnight Saturday around the Duffey; slab avalanches to size 2 were observed on north-northeasterly aspects around ridgetops and in recently loaded lee features on Sunday. Explosives also triggered small (size 1-1.5) wind slab avalanches on north to west aspects about 2000 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small wind slab pockets were reactive to skiers in cross-loaded features at treeline.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase on if the sun shines, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Tuesday indicated no recent avalanche activity. </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">We received a great MIN report from the Shames backcountry that describes an active wet loose avalanche cycle to size 1.5, more details </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/52d2a82b-d285-4609-841c-a969297052de" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">A combination of new snow and wind may increase the reactivity of the existing wind slabs. The sun can really pack a punch this time of year and trigger loose wet avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity reported on Tuesday. </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_AA239A9B">The sun can really pack at punch this time of year and trigger loose wet avalanches, especially on solar aspects. North facing alpine slopes may have the best snow quality, however reactive wind slabs remain possible to trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural and human triggered storm slab avalanches up to size 2.5 were reported on west, north and east aspects in the alpine. A few natural and human triggered wind slabs to size 1.5 were reported from immediate lee features in the alpine. Several natural loose avalanches up to size 2.5 were observed on northerly aspects at treeline and in the alpine.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday and Saturday, there were a few reports of natural and human triggered storm/wind slab avalanches up to size 2 at treeline and alpine elevations. There were also reports of several natural and human triggered loose wet avalanches up to size 1.5 on steep solar slopes and below treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday there was quite a bit of natural avalanche activity in the recent storm snow. Slabs to size 1.5 were reported from all aspects between 1800 and 2700 m. The natural activity was likely caused by the appearance of the strong April sun.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday wind slabs to size 2 released naturally and were also susceptible to human triggering on north, northeast and east facing terrain between 1900 and 2200 m</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, only a few human triggered loose wet avalanches to size 1 were reported.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there were reports of numerous natural, human and explosive triggered storm slab avalanches up to size 2.5 at treeline and in the alpine on all aspects (see this </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/06ce6624-4ca5-45e8-916a-26744aed6d38" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715">).</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered small (size 1-1.5) storm slab avalanches up to 30 cm deep. Skier traffic triggered small pockets of storm snow with the deepest (up to 40 cm) and most reactive deposits in specific lee terrain.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, several natural and human triggered storm/wind slab avalanches 10-50 cm deep and up to size 2.5 were observed on north and east aspects in the alpine. A size 1.5 explosive triggered cornice did not trigger an avalanche on the northeast facing slope below. Several natural loose wet and wet slab avalanches up to size 2 were reported from southeast, south, west and northwest facing slopes (see a MIN report from Glacier National Park </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">). </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural and human triggered loose wet avalanches up to size 2 were observed on sun exposed slopes in the alpine. There were also reports of several natural, human and explosive triggered storm slab avalanches and wind slabs in immediate lee features up to size 2 in the alpine on west, north and east aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, small (size 1-1.5) wind slabs were reactive to skiers, generally around ridge crests and steep, convex terrain above 2200 m. The most reactive deposits were in immediate lee features, including a size 2 wind slab avalanche remotely triggered from a rocky saddle 10 m away. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Overnight Sunday and into Monday, a natural avalanche cycle to size 2 occurred on the western side of the Purcells Forecast region. Storm slab avalanches to size 2, with crowns 20-50 cm deep were observed in alpine terrain on all aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, skiers were able to trigger slabs up to size 1.5 in steep, gully features as low as 2200m. Explosives produced avalanches to size 2 and a helicopter remotely triggered a size 1.5 avalanche from 200 m away, these avalanches all started in steep, alpine terrain above 2400 m, mostly on northerly aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, loose wet avalanches up to size 1 were reported from steep alpine features. Snowfall amounts are uncertain for the next 24 hours and if the region receives more then 15 cm it could increase the avalanche hazard.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region on Wednesday, the following is all from the Lizard Range and Flathead region: </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">On Wednesday, numerous natural loose wet avalanches up to size 1&nbsp; occurred mostly from steep alpine terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, natural storm slab avalanches to size 2 were observed on northerly aspects around 2200-2400 m in the Whistler Backcountry, initiating from steep, lee start zones. Four skier-triggered avalanches (size 1.5-2) in the Whistler Backcountry were reported on Monday, including this Decker Main MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. These similar avalanches occurred in northerly alpine terrain and below a ridge feature.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, avalanche control work with explosives triggered mostly small storm slabs (size 1-1.5) and cornices in alpine and treeline; these avalanches failed on the storm snow - melt-freeze crust interface.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, small (size 1-1.5) storm slabs and wind slabs were reactive to skier traffic. Cornices were reactive to explosives and triggered large (size 2) slab avalanches as they fell on the slopes below. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from Blowdown </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/a1eae6eb-3ee1-47d8-bfe9-63b9554830a1" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a size 2 skier triggered wind slab avalanche on a northeast alpine aspect on Monday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from the Whistler Backcountry </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a similar skier triggered slab avalanche on Monday. The avalanche was triggered in lee-ward terrain below a ridge feature. While outside the forecast region, the avalanche highlights a similar terrain feature that may hold wind slabs in the South Coast Inland.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle to size 2 occurred overnight Saturday around the Duffey; slab avalanches to size 2 were observed on north-northeasterly aspects around ridge crest and in recently loaded lee features on Sunday morning. On Sunday, explosives triggered small (size 1-1.5) wind slab avalanches on north to west aspects about 2000 m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">The likelihood of triggering loose wet avalanches will increase as temperatures rise, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports on Wednesday indicated no recent avalanche activity. </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">A combination of new snow and wind may increase the reactivity of the existing wind slabs. The sun can really pack a punch this time of year and trigger loose wet avalanches especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity reported on Wednesday. </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_AA239A9B">The sun can really pack at punch this time of year and trigger loose wet avalanches, especially on solar aspects. North facing alpine slopes may have the best snow quality, however reactive wind slabs remain possible to trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, several natural, human and remote triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a MIN report from Glacier National Park </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">). </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural and human triggered storm slab avalanches up to size 2.5 were reported on west, north and east aspects in the alpine. A few natural and human triggered wind slabs to size 1.5 were reported from immediate lee features in the alpine. Several natural loose avalanches up to size 2.5 were observed on northerly aspects at treeline and in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On Tuesday, a small (size 1) slab avalanche 30 cm. deep was remotely triggered by a skier from 80 m. away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 where triggered on solar aspects throughout the day by strong solar radiation.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Monday there was quite a bit of natural avalanche activity in the recent storm snow. Slabs to size 1.5 were reported from all aspects between 1800 and 2700 m. The natural activity was likely caused by the appearance of the strong April sun.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Sunday wind slabs to size 2 released naturally and were also susceptible to human triggering on north, northeast and east facing terrain between 1900 and 2200 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a few human triggered wind/storm slabs up to size 1 were observed on sun affected slopes in the alpine. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, only a few human triggered loose wet avalanches to size 1 were reported.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, there were reports of numerous natural, human and explosive triggered storm slab avalanches up to size 2.5 at treeline and in the alpine on all aspects (see this </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/06ce6624-4ca5-45e8-916a-26744aed6d38" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715">).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, no natural avalanche activity was reported. A human triggered wind slab avalanche of size 1.5 on a north aspect at treeline was observed in the south of the region.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 10-50 cm deep and up to size 2.5 were observed on north and east aspects in the alpine. A size 1.5 explosive triggered cornice did not trigger an avalanche on the northeast facing slope below. Several natural loose wet and wet slab avalanches up to size 2 were reported from southeast, south, west and northwest facing slopes (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Wednesday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, skiers were able to trigger slabs up to size 1.5 in steep, gully features as low as 2200m. Explosives produced avalanches to size 2 and a helicopter remotely triggered a size 1.5 avalanche from 200 m away, these avalanches all started in steep, alpine terrain above 2400 m, mostly on northerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, small (size 1-1.5) wind slabs were reactive to skiers, generally around ridge crests and steep, convex terrain above 2200 m. The most reactive deposits were in immediate lee features, including a size 2 wind slab avalanche remotely triggered from a rocky saddle 10 m away. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Overnight Sunday and into Monday, a natural avalanche cycle to size 2 occurred on the western side of the Purcells Forecast region. Storm slab avalanches to size 2, with crowns 20-50 cm deep were observed in alpine terrain on all aspects. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Its important to make observations with changing conditions through the day and know when to pull back or dive into your line. If you're unsure, its best to have a conservative approach.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region on Thursday, the following is from the Lizard Range:</span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Its important to make observations with changing conditions through the day and know when to pull back or dive into your line. If you're unsure, its best to have a conservative approach.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were numerous small (size 1) skier triggered storm slabs reported on primarily northerly aspects below ridgetops near Whistler.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, four skier-triggered storm slab avalanches (size 1.5-2) in the Whistler backcountry were reported on north facing aspects below alpine ridgetops, including this Decker Main MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Wednesday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from Blowdown </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/a1eae6eb-3ee1-47d8-bfe9-63b9554830a1" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a size 2 skier triggered wind slab avalanche on a northeast alpine aspect on Monday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from the Whistler Backcountry </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a similar skier triggered slab avalanche on Monday. The avalanche was triggered  on a northwesterly aspect in lee terrain below a ridge feature. While outside the forecast region, the avalanche highlights the wind slab problem that exists in the South Coast Inland.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, reports indicated several natural slab releases and a cornice fall up to size 2.5. Skier triggered slab avalanches (remotely-from a far) were also reported up to size 1.5. We suspect these avalanches were primarily failing on the April 4th crust interface. Daytime warming produced loose wet avalanches on solar aspects up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche activity reported on Thursday. </span><span class="s_AA239A9B"><br /></span><span class="s_3FE45715">If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_AA239A9B">The sun can really pack at punch this time of year and trigger loose wet avalanches, especially on solar aspects. North facing alpine slopes may have the best snow quality, however reactive wind slabs remain possible to trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday the avalanche activity decreased. A few natural and human triggered wind/storm slab avalanches up to size 2 were reported on west and north aspects at treeline and in the alpine. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Two of these were remotely triggered, one by humans and another one by a helicopter. A layer of small surface hoar below the most recent snow may have been the weak layer. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park). </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, no new avalanche activity was observed. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a small (size 1) slab avalanche 30 cm deep was remotely triggered by a skier from 80 m away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 were triggered on solar aspects throughout the day by strong solar radiation.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday there was quite a bit of natural avalanche activity in the recent storm snow. Slabs to size 1.5 were reported from all aspects between 1800 and 2700 m. The natural activity was likely caused by the appearance of the strong April sun. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, only a few explosive triggered wind slab avalanches were reported. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a few human triggered wind/storm slabs up to size 1 were observed on sun affected slopes in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, only a few human triggered loose wet avalanches to size 1 were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new from the past few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day, especially in areas with fresh snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday no new avalanche activity was observed. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday no natural avalanche activity was reported. A human triggered wind slab avalanche of size 1.5 on a north aspect at treeline was observed in the south of the region.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 10-50 cm deep and up to size 2.5 were observed on north and east aspects in the alpine. A size 1.5 explosive triggered cornice did not trigger an avalanche on the northeast facing slope below. Several natural loose wet and wet slab avalanches up to size 2 were reported from southeast, south, west and northwest facing slopes (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Thursday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, skiers were able to trigger slabs up to size 1.5 in steep, gully features as low as 2200m. Explosives produced avalanches to size 2 and a helicopter remotely triggered a size 1.5 avalanche from 200 m away. They initiated in steep, alpine terrain above 2400 m, mostly on northerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, small (size 1-1.5) wind slabs were reactive to skiers, generally around ridge crests and steep, convex terrain above 2200 m. The most reactive deposits were in immediate lee features, including a size 2 wind slab avalanche remotely triggered from a rocky saddle 10 m away. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Its important to make observations with changing conditions through the day and know when to pull back or dive into your line. If you're unsure, its best to have a conservative approach.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region on Thursday, the following is from the Lizard Range:</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Its important to make observations with changing conditions through the day and know when to pull back or dive into your line. If you're unsure, its best to have a conservative approach.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, there were numerous small (size 1) skier triggered storm slabs reported on primarily northerly aspects below ridgetops near Whistler. Avalanche activity is expected to increase on Saturday with the forecast snow and wind.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, four skier-triggered storm slab avalanches (size 1.5-2) in the Whistler backcountry were reported on north facing aspects below alpine ridgetops, including this Decker Main MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Thursday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from Blowdown </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/a1eae6eb-3ee1-47d8-bfe9-63b9554830a1" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a size 2 skier triggered wind slab avalanche on a northeast alpine aspect on Monday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A MIN report from the Whistler Backcountry </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715"> documents a similar skier triggered slab avalanche on Monday. The avalanche was triggered on a northwesterly aspect in lee terrain below a ridge feature. While outside the forecast region, the avalanche highlights the wind slab problem that exists in the South Coast Inland.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday small loose wet avalanches were observed in steep terrain. Control work produced a few storm slab avalanches to size 2 on northeast facing slopes between 1800 and 2000 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, reports indicated several natural slab releases and a cornice fall up to size 2.5. Skier triggered slab avalanches (remotely-from a far) were also reported up to size 1.5. We suspect these avalanches were primarily failing on the April 4th crust interface. Daytime warming produced loose wet avalanches on solar aspects up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday small loose wet avalanches were reported from steep terrain. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a few human triggered loose wet avalanches up to size 1.5 were observed on steep slopes in the afternoon. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday the avalanche activity decreased. A few natural and human triggered wind/storm slab avalanches up to size 2 were reported on west and north aspects at treeline and in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Two of these were remotely triggered, one by humans and another one by a helicopter. A layer of small surface hoar below the most recent snow may have been the weak layer. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a couple natural and machine triggered storm slab avalanches 20-40 cm deep and up to size 2.5 were observed on east facing alpine slopes.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, no new avalanche activity was observed.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a small (size 1) slab avalanche 30 cm deep was remotely triggered by a skier from 80 m away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 were triggered on solar aspects throughout the day by strong solar radiation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, no new avalanche activity was observed. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, only a few explosive triggered wind slab avalanches were reported.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a few human triggered wind/storm slabs up to size 1 were observed on sun affected slopes in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region on Thursday. However, avalanche activity is expected to increase on Saturday with the forecast snow and wind.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday morning, a size 2 storm slab was observed in a wind-loaded pocket on a west aspect in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, a skier triggered wind slab avalanche of size 1.5 on a north aspect at treeline was reported in the south of the region.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 10-50 cm deep and up to size 2.5 were observed on north and east aspects in the alpine. A size 1.5 explosive triggered cornice did not trigger an avalanche on the northeast facing slope below. Several natural loose wet and wet slab avalanches up to size 2 were reported from southeast, south, west and northwest facing slopes (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, explosive cornice control work dropped a large cornice on a rocky slope which triggered a size 2.5 slab avalanche 50 cm deep on a northeast aspect.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, skiers were able to trigger slabs up to size 1.5 in steep, gully features as low as 2200m. Explosives produced avalanches to size 2 and a helicopter remotely triggered a size 1.5 avalanche from 200 m away. They initiated in steep, alpine terrain above 2400 m, mostly on northerly aspects.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday small loose wet natural avalanches were reported from steep south facing terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region, the following is from the Lizard Range:</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday small loose wet natural avalanches were reported from steep south facing terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, explosive control was able to initiate a few loose dry avalanches up to size 1.5 which failed in the recent storm snow. In the afternoon skier controlled loose wet avalanches were easily triggered at treeline and below up to size 1.5 on sunny aspects. No natural avalanche activity was reported and no new avalanches were noted in alpine elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday small (size 1) storm slabs were reactive to skier traffic, primarily in lee terrain below ridgetops.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, four skier-triggered storm slab avalanches (size 1.5-2) in the Whistler backcountry were reported on north facing aspects below alpine ridgetops, including this Decker Main MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/c0281b43-3f36-40ec-9439-584b61db7b3b" target="_blank"><span class="s_B5813F7D">here</span></a><span class="s_3FE45715">. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small (size 1) skier triggered loose wet avalanches were reported in the Duffey Lake area on Friday. Small wind slabs are expected to be the primary concern on Sunday with the forecast snow and wind.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">We received a great </span><a href="https://www.avalanche.ca/map/forecasts/northwest-coastal?panel=mountain-information-network-submissions/c9ea1c6e-acf4-405b-bcba-78f6f0e1b926" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715"> on Friday. It details a few avalanche occurrences including a size 3 on an east facing slope and lots of loose wet activity from steep terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday small loose wet avalanches were observed in steep terrain. Control work produced a few storm slab avalanches to size 2 on northeast facing slopes between 1800 and 2000 m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, reports indicated several natural slab releases and a cornice failure up to size 2.5. Slab avalanches were remotely triggered (from a distance) by riders up to size 1.5. We suspect these avalanches were running on the April 4th crust interface. Daytime warming produced loose wet avalanches on solar aspects up to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">The last reported avalanche activity came on Thursday when small loose wet avalanches were reported from steep terrain. If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a few human triggered loose wet avalanches up to size 1.5 were observed on steep slopes in the afternoon. Evidence of a solar-induced wet slab cycle on west aspect around 2400 m was reported on Friday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday the avalanche activity decreased. A few natural and human triggered wind/storm slab avalanches up to size 2 were reported on west and north aspects at treeline and in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Two of these were remotely triggered, one by humans and another one by a helicopter. A layer of small surface hoar below the most recent snow may have been the weak layer. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a couple natural and machine triggered storm slab avalanches 20-40 cm deep and up to size 2.5 were observed on east facing alpine slopes.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a small (size 1) slab avalanche 30 cm deep was remotely triggered by a skier from 80 m away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 were triggered on solar aspects throughout the day by strong solar radiation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, wind slabs in lee features were reactive to explosives.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, wind and storm slabs up to size 1 were reactive to skier traffic on sun affected slopes in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the region on Friday. However, avalanche activity is expected to increase on Sunday with the new snow and wind.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Late Saturday, storm snow was sluffing in steep terrain with skier traffic and gaining cohesion.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday morning, a size 2 storm slab was observed in a wind-loaded pocket on a west aspect in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, a skier triggered wind slab avalanche of size 1.5 on a north aspect at treeline was reported in the south of the region.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 10-50 cm deep and up to size 2.5 were observed on north and east aspects in the alpine. A size 1.5 explosive triggered cornice did not trigger an avalanche on the northeast facing slope below. Several natural loose wet and wet slab avalanches up to size 2 were reported from southeast, south, west and northwest facing slopes (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, explosive cornice control work dropped a large cornice on a rocky slope which triggered a size 2.5 slab avalanche 50 cm deep on a northeast aspect.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle occurred Saturday night, the highlights were storm slabs up to size 2 on northeast facing alpine terrain around 1700 m. A natural cornice failure was observed from a north facing ridgeline which subsequently triggered a size 2.5 storm slab involving the new snow. Control work produced storm slabs to size 2.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We received a </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/d5df01eb-fe4c-4448-9022-d2a11a82846a" target="_blank"><span class="s_B5813F7D">great MIN report</span></a><span class="s_3FE45715"> of a small storm slab from Saturday morning, and this was well before the storm really kicked into gear. On Friday small loose wet natural avalanches were reported from steep south facing terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region, the following is from the Lizard Range:</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle occurred Saturday night, the highlights were storm slabs up to size 2 on northeast facing alpine terrain around 1700 m. A natural cornice failure was observed from a north facing ridgeline which subsequently triggered a size 2.5 storm slab involving the new snow. Control work produced storm slabs to size 2.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We received a </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/d5df01eb-fe4c-4448-9022-d2a11a82846a" target="_blank"><span class="s_B5813F7D">great MIN report</span></a><span class="s_3FE45715"> of a small storm slab from Saturday morning, and this was well before the storm really kicked into gear. Storm slabs likely ran through the night and into Sunday, we should have more details to report on Monday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday small (size 1) storm slabs were reactive to skier traffic, primarily in lee terrain below ridgetops.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported in this region on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a snowmobiler was buried in a size 2.5 wind slab avalanche on a north facing aspect at 2200 m. near the Blowdown cabin. Check out the MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/573f7540-41dc-46bc-a893-32d270d673cb" target="_blank"><span class="s_B5813F7D">HERE. </span></a><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Ne new avalanche activity to report from yesterday, but most of the snow fell late in the day.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We received a great </span><a href="https://www.avalanche.ca/map/forecasts/northwest-coastal?panel=mountain-information-network-submissions/c9ea1c6e-acf4-405b-bcba-78f6f0e1b926" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715"> on Friday. It details a few avalanche occurrences including a size 3 on an east facing slope and lots of loose wet activity from steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent reported avalanche activity has been limited to small loose wet sluffing from gulley walls below treeline. Avalanches were also heard, but not seen running from big unskiable terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Late Saturday, storm snow was sluffing in steep terrain with skier traffic and gaining cohesion.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a few human triggered loose wet avalanches up to size 1.5 were observed on steep slopes in the afternoon. Evidence of a solar-induced wet slab cycle on west aspect around 2400 m was reported on Friday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday the avalanche activity decreased. A few natural and human triggered wind/storm slab avalanches up to size 2 were reported on west and north aspects at treeline and in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, several natural and human triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Two of these were remotely triggered, one by humans and another one by a helicopter. A layer of small surface hoar below the most recent snow may have been the weak layer. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/875d8b29-2453-4545-8a8e-0e451498aae1" target="_blank"><span class="s_9255B882">MIN report</span></a><span class="s_AA239A9B"> from Glacier National Park).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a couple natural and machine triggered storm slab avalanches 20-40 cm deep and up to size 2.5 were observed on east facing alpine slopes.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, a small (size 1) slab avalanche 30 cm deep was remotely triggered by a skier from 80 m away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 were triggered on solar aspects throughout the day by strong solar radiation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Late in the day Sunday, small wind slab pockets were reactive to skier traffic.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, wind slabs in lee features were reactive to explosives.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, wind and storm slabs up to size 1 were reactive to skier traffic on sun affected slopes in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, numerous small (size 1) skier triggered storm slab avalanches were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday, a skier triggered a size 1.5 wind slab avalanche on a steep convex roll at 2150 m and explosives triggered a size 2 storm slab avalanche at 2350, both avalanches occurred on a northeast aspect. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche Sunday was also observed north aspect at 2300 m. The size 2 storm slab avalanche failed on surface hoar likely buried early April. This isolated layer may see increased stress as winds redistribute snow and add load or temperatures penetrate the snowpack.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Late Saturday, storm snow was sloughing in steep terrain with skier traffic and gaining cohesion.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small to large (size 1 to 2) storm slab avalanches were reported on Sunday. They were in alpine terrain, around 30 cm deep, and on north to west aspects. Otherwise, the recent loose storm snow was reactive to skier traffic on steep, southerly aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday skier triggered avalanches were widespread on north through east facing slopes in the alpine and down into treeline too.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle occurred Saturday night, the highlights were storm slabs up to size 2 on northeast facing alpine terrain around 1700 m. A natural cornice failure was observed from a north facing ridgeline which subsequently triggered a size 2.5 storm slab involving the new snow. Control work produced storm slabs to size 2. We received a </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/d5df01eb-fe4c-4448-9022-d2a11a82846a" target="_blank"><span class="s_B5813F7D">great MIN report</span></a><span class="s_3FE45715"> of a small storm slab from Saturday morning, and this was well before the storm really kicked into gear. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from this region, the following is from the Lizard Range:</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday storm slabs were quite sensitive to human triggering to size 2 on north through east facing slopes in the alpine and down into treeline. A little further down into treeline the snowpack was well bonded to the old crust, check out </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/9ab8b99e-e0ea-40ae-abee-5f1402e72081" target="_blank"><span class="s_B5813F7D">this MIN report</span></a><span class="s_3FE45715"> for more details.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle occurred Saturday night, the highlights were storm slabs up to size 2 on northeast facing alpine terrain around 1700 m. A natural cornice failure was observed from a north facing ridgeline which subsequently triggered a size 2.5 storm slab involving the new snow. Control work produced storm slabs to size 2. We received a </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/d5df01eb-fe4c-4448-9022-d2a11a82846a" target="_blank"><span class="s_B5813F7D">great MIN report</span></a><span class="s_3FE45715"> of a small storm slab from Saturday morning, and this was well before the storm really kicked into gear.&nbsp; </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous small to large (size 1 to 2) storm and wind slab avalanches were reported in the region on Sunday. They were triggered naturally, by skiers, and explosives. They were most often in alpine terrain and released within the recent storm snow, between 20 and 40 cm deep.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives triggered small cornice chunks on northerly ridges on Monday. The chunks did not trigger slabs on the slopes below.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">If you have any recent observations during your travels, we would greatly appreciate it if you posted a photo or any other information to the </span><a href="https://www.avalanche.ca/mountain-information-network/submit" target="_blank"><span class="s_B5813F7D">Mountain Information Network (MIN)</span></a><span class="s_3FE45715">. Thanks!</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Ne new avalanche activity to report from Saturday or Sunday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">We received a great </span><a href="https://www.avalanche.ca/map/forecasts/northwest-coastal?panel=mountain-information-network-submissions/c9ea1c6e-acf4-405b-bcba-78f6f0e1b926" target="_blank"><span class="s_B5813F7D">MIN report</span></a><span class="s_3FE45715"> on Friday. It details a few avalanche occurrences including a size 3 on an east facing slope and lots of loose wet activity from steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday natural wind slabs to size 1.5 were observed on northeast facing slopes between 1400 and 1800 m. A natural cornice failure produced a size 2.5 wind slab when it impacted the underlying slope.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday loose wet sluffing from gulley walls was reported below treeline. Avalanches were also heard, but not seen running from big unskiable terrain.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">If you're out we'd love it if you would submit what you're seeing to the </span><a href="https://www.avalanche.ca/mountain-information-network#give-information" target="_blank"><span class="s_B5813F7D">Mountain Information Network.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday, two size 2 storm slab avalanches were triggered by skiers on east aspects at 2200m. A group of skiers remote triggered a size 2 storm slab avalanche from 50 m away, failing on a southeast slope at 2250 m. One natural size 2 storm slab avalanche was observed on a steep, north aspect between 2100-2550 m. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Late Saturday, storm snow was sloughing in steep terrain with skier traffic and gaining cohesion.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday a small (size 1) natural storm slab was observed on an east aspect at 2600 m.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, a couple natural and machine triggered storm slab avalanches 20-40 cm deep and up to size 2.5 were observed on east facing alpine slopes.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Last Tuesday, a small (size 1) slab avalanche 30 cm deep was remotely triggered by a skier from 80 m away on a northeast aspect at 2250 m. A layer of small surface hoar below the most recent snow may have been the weak layer. Additionally, several loose wet avalanches up to size 1.5 were triggered on solar aspects throughout the day by strong solar radiation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday, several small size 1 wind slabs were reactive to explosives, one size 3 wind slab avalanche was triggered with a very large explosive. Near Whitewater a skier triggered a windslab avalanche on a steep northwest aspect in the alpine. See the MIN report </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/22af0f64-dd48-49ab-9fdb-f8df658ac65b" target="_blank"><span class="s_9255B882">here</span></a><span class="s_AA239A9B">. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_B5813F7D { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Sunday. If you have any recent observations during your travels, we would greatly appreciate it if you posted a photo or any other information to the </span><a href="https://www.avalanche.ca/mountain-information-network/submit" target="_blank"><span class="s_B5813F7D">Mountain Information Network (MIN)</span></a><span class="s_3FE45715">. Thanks!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">When winds picked up there was a sz 1.5 sluff out of steep ski terrain in the Granddaddy couloir on Bow Peak.  Not much mass but would have flushed a skier or climber.  Lake Louise ski hill had no results bombing in previously uncontrolled terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Poor visibility prevented any observations but an avalanche was heard in the Hilda creek area originating from steep unskiable alpine terrain which has a Northeasterly aspect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 natural size 2 avalanches were obersved adjacent to the highway yesterday. They were on N aspects, starting at eleveations of 22-2800 m, and ran into the avalanche fans. Cheops N4 (aka STS couloir) ran naturally on Thursday into the avalanche fan. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A size 3 slab was observed in the Hilda creek area. It originated from sloughing in a gully feature and expanded into a slab on a large open slope at 2400m that is the run out for the gully.  The slab likely propogated on facets around the November 01 rain crust. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, distinct avalanche cycles occurred during periods of intense loading by wind and snow. 1 size 3 and 22 size 2-2.5 natural avalanches were observed from paths above the highway, east of Rogers Pass. These occurred from steep complex terrain, some avalanching repeatedly. Skiers reported seeing an avalanche in &quot;frequent flyer&quot; path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous Class 1-1.5 ski cut slabs in the alpine (25-40 cm deep) were reported by Sunshine ski patrol today. Yesterday climbers reported a sizable slide on Polar Circus ice climb running down to below the pencil feature.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A size 3 slab was observed in the hilda creek area. It originated from sloughing in a gully feature and expanded into a slab on a large open slope at 2400m that is the runout for the gully.? The slab likely propogated on the November 01 raincrust. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has been occurring from steep complex terrain during periods of intense wind and snowfall. Most are size 2-2.5, and several paths have run repeatedly, some running to the end of their runouts. There have been reports of natural avalanches from the Cheops north paths. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No New avalanche observations due to obscured visibility.  On Saturday, a size 3 slab was observed in the hilda creek area. It originated from sloughing in a gully feature and expanded into a slab in the runout at 2400m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday an avalanche cycle occurred during a period of intense wind and snowfall. 6 size 3, and 13 size 2-2.5 natural avalanches were observed from steep paths adjacent to the highway, east of the Summit. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity has centered around extreme terrain in the immediate lee areas from  recent winds. Visibility has been poor in the last 48-hours with fog and precipitation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surprisingly little slab activity reported or observed today. Some storm soft slabs to size 2 were reported along HWY 93 N.&nbsp; A size 2 came off Bourgeau Left ice climb yesterday evening and again today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No New avalanche observations due to obscured visibility.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, distinct avalanche cycles occurred during periods of intense wind and snowfall. 1 size 3 and 22 size 2-2.5 natural avalanches were observed from paths adjacent to the highway, east of Rogers Pass. These all occurred from steep terrain...</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive control on Sunshine Road only produced 1 sz.2.5 on Mount Bourgeau (NE asp, 2500m)&nbsp; </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.facebook.com/photo.php?fbid=442693632447298&amp;set=a.433664953350166.91114.145133538869977&amp;type=3&amp;theater" target="_blank"><span class="s_9255B882">(photo)</span></a><span class="s_AA239A9B"> </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.facebook.com/photo.php?fbid=447700325290612&amp;set=a.437654162961895.101998.219810324746281&amp;type=3&amp;theater" target="_blank"><span class="s_9255B882">(francais)</span></a><span class="s_AA239A9B"> which stepped to the Nov 6 crust and was approx.1m deep. Forecasters on Crowfoot peak saw 1 sz.3 &amp; 1 sz.2  on high NE facing terrain on Vulture Peak which in spots stepped to glacial ice within the last 48-72 hrs. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No New significant natural avalanches were observed today. Explosive work along parkers slabs with 14 avalauncher shots only produced one size 2 slab avalanche from a windloaded location on rock slab.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, distinct avalanche cycles occurred during periods of intense wind and snowfall. 1 size 3.5 and 2 size 2-2.5 natural avalanches were observed from paths adjacent to the highway. Notably some of the avalanches observed yesterday ran right to the valley bottom.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few avalanches have been seen out of extreme terrain on the lee sides of exposed ridges. These events may have been triggered by sloughing off of steep terrain or by cornice failures. Although the sizes of these events have been small they have traveled a long way in confined terrain: gullies and couloirs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches in the past 24 hrs. Storm related avalanches from the last week to size two in wind effected areas. Explosive control to size 3 stepping down to Nov. Crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No new natural avalanches were observed today. Explosive work along Parker slabs with produced one size 2.5 slab avalanche from a wind loaded location on rock slab on Thursday.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little activity observed yesterday considering 15cm HN and past high to extreme winds.  No new avals were observed along the highway corridor or in the Mt. Fidelity area.  Minimal sluffing observed skiing steep sheltered slopes at all elevations.  A medium avalanche cycle occured on Wednesday concentrated to the steep terrain east of Rogers Pass.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed. On a flight today over the Wapta and Vermilion, several large size 2.5-3 full depth releases were observed that were approximately 3-4 days old. We suspect these failed on the Nov. crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Good visibility today. Three size 2-2.5 avalanches were noted 24-48 hrs old, 40 degree plus, NW aspect, cross loaded gullys. Explosive work on parkers slabs on Thursday with 22 avalauncher rounds produced one size 2 slab avalanche in a windloaded location on smooth steep rock slab. Settlement and localized winds are creating pockets of slabs. ? </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avals were observed in the last two days along the highway corridor.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Wednesday, a natural avalanche cycle occurred with, 1 size 3.5 and 2 size 2-2.5 avalanches observed from paths adjacent to the highway, east of Rogers Pass.&nbsp; Avalanche started in steep terrain east of the summit, with some depositing snow at the end of runnout.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed or reported today. However, there have been reports and observations of avalanches up to size 3 throughout the forecast region in the past 4 days. It is suspected that many of these large avalanche released on the Nov 6th crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday three size 2-2.5 avalanches were noted now 48-72 hours old, 40 degree plus, NW aspect, cross loaded gullies. Thursday' s explosive work on parkers slabs with 22 avalauncher rounds produced one size 2 slab avalanche in a wind loaded location on smooth steep rock slab. Patrol South today had limited visibility but swirling winds encountered. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">3 Loose natural sz 2.0 avalanches observed off of the N face of Mt Macdonald from early yesterday morning</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 sz 1.0 natural from video peak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size two avalanche was observed high on Bourgeau 8, above the Bourgeau Left ice climb. It is suspected to be a recently developed wind slab from todays wind event. No other avalanches were observed or reported. </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.facebook.com/photo.php?fbid=444288548954473&amp;set=a.433664953350166.91114.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Photo of avalanche in Bourgeau 8.</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday three size 2-2.5 avalanches were noted now 48-72 hours old, 40 degree plus, NW aspect, cross loaded gullys. Explosive work on parkers slabs on Thursday with 22 avalauncher rounds produced one size 2 slab avalanche in a windloaded location on smooth steep rock slab. Expect current winds to  increase potential for natural avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 Natural size 2.0 loose avalanches were observed yesterday morning in the north acing gullies of Mt Macdonald.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.   There is certainly potential for skier triggered wind slab avalanches at treeline and in the alpine.  Watch for steep wind loaded terrain or thin areas which may be weaker than the surrounding snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche cycle has occurred in the past 24-48 hrs.  Slab avalanches to size 3 have occurred on E to W aspects at alpine and tree line elevations and have stepped down to the basal facet layer.  Large cornice failure has triggered large avalanches on the basal facet layer as well.  Winds will ease, however, expect touchy conditions to continue.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 Natural size 3.0 slab on Mt Green.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">4 Natural size 2.5 slab release in the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sluffing to size 1 was observed in the last 24 hours from steeper, NE-facing slopes. Evidence of an old skier-triggered slide near Observation Peak in a cross-loaded gully. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche cycle occurred Sunday into Monday.  Slab avalanches to size 3 were observed on NE aspects at alpine and tree line elevations and in some locations, have stepped down to the basal facet layer.  Large cornice failure has triggered large avalanches on the basal facet layer as well. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few isolated natural avalanches were observed from steep terrain yesterday, mostly from north aspects.  Avalanche control produced several slab avalanches up to size 3.5.  Most of these were high elevation targets where cross loading was a factor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of cornice triggered size 1-1.5 slab avalanches, 20-40 cm thick, in the last 24 hours above the Bourgeau left ice climb (SE asp) near Sunshiine.  They ran quite far for their mass, but stopped about 150 m above the climb.  No other new avalanches reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported since the end the cycle that ended on Monday.  In that cycle, slab avalanches to size 3 were observed on NE aspects at alpine and tree line elevations, several stepped down to the basal facet layer.  Large cornice failure triggered large avalanches on the basal facet layer as well.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little avalanche activity has been observed in the past few days.  Avalanches which have been observed are mostly from steep alpine start zones affected by wind.  Wind affected and cross loaded features, and thin areas are most likely to produce human triggered avalanches.  Some loose snow sluffing has also been observed in steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little natural activity to speak of although there are some ripe looking start zones waiting for a trigger. Cornices also are continuing to grow and many look fragile.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today and very little activity in the past week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported since the end the cycle that ended on Monday.  In that cycle, slab avalanches to size 3 were observed on NE aspects at alpine and tree line elevations, several stepped down to the basal facet layer.  Large cornice failure triggered large avalanches on the basal facet layer as well.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little avalanche activity has been observed in the past few days.? Avalanches which have been observed are mostly from steep alpine start zones affected by wind and some sluffing below cornices on steep N and E aspects.? Wind affected and cross loaded features, and thin areas are most likely to produce human triggered avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the past 24 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported since the end the cycle that ended on Monday.? In that cycle, slab avalanches to size 3 were observed on NE aspects at alpine and tree line elevations, several stepped down to the basal facet layer.? Large cornice failure triggered large avalanches on the basal facet layer as well.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One new natural avalanche was observed along the highway. This size 2 loose avalanche was from a steep north facing alpine start zone affected by wind. Avalanche technicians traveling in the Illecillewaet and Asulkan drainages observed no new avalanches, nor did they experience any sluffing while skiing steep S and W slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some very small skier controlled slabs on north and east ridges with the new thin wind slab development, otherwise no new avalanches in the last 24 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed since Monday Dec 10.  Wind slabs appear to have bonded well to the old snow surface. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">With no new snow and light winds yesterday, no new avalanches were observed. On Friday, avalanche technicians traveling in the Illecillewaet and Asulkan drainages observed no new avalanches, nor did they experience any sluffing while skiing steep S and W facing slopes. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Heard one avalanche that likely came out of extreme terrain at the back of the Cameron Lake area. Only surface sloughing observed today with ski cutting but we stayed in conservative terrain. Many start zones look to be quite loaded and waiting for a trigger...</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today by forecasters during a flight of the highway avalanche control paths as well as a team in the Lake O'hara area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed since Monday Dec 10.  Wind slabs appear to have bonded well to the old snow surface. The raincrust laminate down in the lower 1/3 of snowpack is deteriorating into a FC layer and does not respond to a compression test.  Test results do show non planar collapses in the basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. Avalanche technicians traveling over Little Sifton and into the Hermit Meadows area found 10cm thick windslabs on convex features that were easily triggerable to size 1 above 2300m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today by forecasters during a field trip in the Lake Louise ski hill backcountry.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several slab and loose avalanches to size 2 occurred on alpine solar aspects originating out of steep rock bands and initiating cross loaded gully features in the Icefields area today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday avalanches were observed up to size 3, and were dry slabs running to 1/2 fan. Expect more dry avalanche activity due to the moderate to strong southerly winds overnight.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today by forecasters during a field trip in the Sunshine ski hill backcountry.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed in the past 24 hours. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday avalanches were observed up to size 2.5, and were dry slabs running to 1/4 fan.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations by Parks staff today.  Reports of ski cutting soft slabs in wind loaded areas by ski patrol at Sunshine and loose snow sluffing out of steep terrain with increased winds.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday No new avalanches were observed in Glacier National Park.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed over the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 size 3 naturals on the N. face of Mt. Victoria within the last 24 hours, initiating at 3000-3300m  It is suspected wind loading caused the snowpack to fail on glacial ice or old firn snow,  No other avalanches of this magnitude observed or reported.  Size 1-1.5 skier controlled avalanches reported at Sunshine ski area limited to ridge crests.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural loose snow avalanches have been reported on steep slopes below tree line where the snowpack is thin.  Loose snow avalanches to size 2 were the result of avalanche control work on the Parkway on December 21st.  The control work was on thin steep below tree line slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Periods of strong southerly winds triggered large natural avalanches from steep, lee avalanche paths overnight.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Friday's avalanche control work at the Icefields released several loose size 2 avalanches in thin steep snowpack areas below treeline. Natural avalanches have been limited to similar characteristics, steep, rocky, thin areas creating loose avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm thick windslabs are reactive to human triggering on convex rolls and unsupported terrain at treeline and above. These avalanches were reported to be size 1's: 20-30m wide and 30m long. Overnight on Thursday, numerous size 2-3 natural slab avalanches were triggered by wind loading on steep N thru E aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Friday's avalanche control work at the Icefields released several loose size 2 avalanches in thin steep snowpack areas below treeline. Natural avalanches have been limited to similar characteristics, steep, rocky, thin areas creating loose avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers triggered very soft slabs on steep north aspects. They were triggered from lee and crossloaded features; just below ridge crest on a gully. The avalanches were size 1-1.5, 20-30cm deep and propagated 30m wide. They ran about 100m.  Also, 3 natural size 2 avalanches were observed from north aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surprisingly little avalanche activity has been observed with all the new snow.  Loose snow avalanches up to size 1.5 have been observed out of very steep terrain at tree line and in the alpine.  A couple of soft slabs up to size 2 have been seen out of steep wind loaded terrain at ridge crests, failing within the recent storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Friday's avalanche control work at the Icefields released several loose size 2 avalanches in thin steep snowpack areas below treeline. Natural avalanches have been limited to similar characteristics, steep, rocky, thin areas creating loose avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday there were 11 natural avalanches observed east of the Roger's Pass summit, sizes ranging from 2.0 to 2.5.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.0 low elevation glide crack release on the south side Mt Cheops.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sluffing and soft slabs out of very steep terrain up to size 2 were observed in the last 24hrs due to the large amount of new snow recently.  No new avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Friday's avalanche control work at the Icefields released several loose avalanches up to size 2, from very steep terrain with thin snow cover at treeline. The few natural avalanches that have been observed share the same characteristics. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One new avalanche size 1.5 avalanche was noted in the highway corridor yesterday.  A size 2.0 low elevation glide crack release on the south side Mt Cheops two days ago.&nbsp; Cornices are getting very large, and could provide the large trigger needed to release avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flight to Bow Summit and to Field in good visibility today showed very little in the way of recent natural avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small slab avalanches to size 1.5 have been observed on steep shallow slopes around tree line on NE aspects.  Small loose snow avalanches have been observed today on steep shallow south facing slopes below tree line. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Very few avalanches noted in the highway corridor over the past few days.  This lack of natural activity is a good indicator that the snowpack is mostly stable.  Some surface sluffing from skiers has also been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flight to Bow Summit and to Field in good visibility on Thursday showed very little in the way of recent natural avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface facets have created numerous small loose avalanches at tree line and above in the Icefields area.  These slides have little mass and have not as yet triggered the wind slabs beneath them.  No natural slab avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A small avalanche cycle was noted yesterday, likely from overnight winds on Dec. 25.  These slides were predominantly on steep terrain from alpine start zones.  Some surface sluffing from skiers has also been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No new avalanches have been observed in the past several days however we expect to see some cornice failures and wind triggered avalanches over the next few days as the winds increase.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche observations in the last 24 hours.  Mainly stable snowpack at the moment, especially West of the divide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the past 2 days, surface facets have created numerous small loose avalanches at tree line and above in the Icefields area.  These slides have little mass and have not as yet triggered the wind slabs beneath them.  No natural slab avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Yesterday we observed two natural avalanches out of steep terrain east of Rogers Pass.  A small avalanche cycle occurred on Wednesday, likely from overnight winds on Dec. 25. Skiers are reporting fast moving surface sluffing in low density HN and faceted snow in the upper pack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported in the last 24 hours from numerous areas and operations. A report on the Wapta from Friday saw several large cornice failures in high alpine terrain which caused either no result or sloughing.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small, loose snow avalanches continue to run from rock bands and steep alpine terrain. These slides have little mass and have not as yet triggered the wind slabs beneath them.? No natural slab avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lake Louise ski area reported a small, skier triggered avalanche in a steep, thin treeline area today.  This was a loose dry avalanche in an area with a completely facetted snowpack. In a deeper snowpack area, a large cornice failure was reported above the Bourgeau LH ice climb, but did not trigger a slab.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Near surface faceting and a clear sunny day produced numerous loose snow avalanches to size 1.5 in the Columbia Icefield Area today. These slides originated from steep, shallow and rocky terrain in the alpine on solar aspects. No new slab avalanches observed on road patrol from Jasper to Sask Crossing (very good visibility).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 size 2 natural loose avalanches yesterday east of the Rogers Pass summit.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a guide reported evidence of a fresh loose dry avalanche on the ice climb 'Rogans Gully' on Cascade mountain. Be wary of loose dry avalanches in steep terrain as the snowpack continues to facet. Otherwise no new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Near surface faceting and a sunny day produced numerous loose snow avalanches to size 1.5 in the Columbia Icefield Area yesterday. These slides originated from steep, shallow and rocky terrain in the alpine on solar aspects.  Cornice control yesterday at Marmot Basin did not trigger any slabs in slopes below. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skiers report sluffing of the top 20cm on steep slopes.  There were no new natural avalanches observed yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span><span class="s_1681A555">Avalanche activity in loaded lee alpine features over the past 48hrs. Likely triggered with light loads, probably sluffs from steep terrain above. Depth 0.5-1m but not steeping down to Nov 6 mfc. Aspects ranging from E to NW.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Human triggering of hard slabs up to 50 cm is a possibility.  Radiation on steep southerly aspects may result in loose snow avalanche that can be a factor in confined features such as waterfall ice routes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the icefields area today. Cooler temperatures and light clouds reduced the number of loose snow avalanches occurring on steep rocks. Cornice control on Sunday at Marmot Basin did not trigger any slabs in the slopes below. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Direct morning sun on easterly aspects caused a large chunk of cornice to fail on Cheops Mtn, triggering a size 2 slab. Small, loose avalanches also ran during this period from steep solar aspects, before clouds moved in reducing the solar effects. Skiers report sluffing of the top 20cm on steep slopes. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the icefields area today. The number of loose snow avalanches has dropped due to the high overcast clouds reducing the solar affect.  Some sloughing has occurred on high alpine rock slabs in steep unskiable terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Direct morning sun on easterly aspects caused a large chunk of cornice to fail on Cheops Mtn, triggering a size 2.5 slab on the 31st. Skiers reported sluffing of the top 20cm on steep slopes. A small slab was ski cut at Balu Pass on an East aspect yesterday down 10-15cm.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A sunshine snow safety team member triggered a cornice while approaching the ridge to do cornice control.  The cornice dropped onto steep terrain, triggering a size 2 that failed on a recent wind slab layer.  Otherwise, no new avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today though expect some loose snow sluffing on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent activity has been confined to steep unskiable terrain. Small, loose avalanches also ran during this period from steep solar aspects, before clouds moved in reducing the solar effects. Skiers report sluffing of the top 20cm on steep slopes. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity over the past two days.  We did see several avalanches up to size 3 out of steep wind loaded alpine terrain a few days ago.  These appeared to be cornice triggered and failing on deeper buried facet layers.&nbsp; This remains a concern especially in areas where the snowpack depth varies substantially.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Yesterday, the combination of the inversion and sun affect led to some notable avalanches in ice climbing terrain on solar aspects along the parkway (outside of our forecast region), to see the details google the mountain condition report, thanks for the report.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today though expect some loose snow sluffing on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent natural avalanche activity observed along the highway corridor has been confined to steep unskiable terrain. Small, loose avalanches triggered by solar radiation have been observed from steep solar aspects.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small loose snow avalanches triggered by skiers in very steep terrain at treeline in the Kootenay region.  Some small loose snow avalanches also noted from steep features in the alpine on solar aspects from the last 24 hrs. All were maximum sz. 1</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche patrols were conducted on both the Maligne Road and the Icefields Parkway.  No new avalanches were observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed one natural loose avalanche yesterday west of the summit on a west aspect along the highway corridor.  Recent natural avalanche activity has been confined to steep unskiable terrain.  Backcountry skiers are reporting large sluffs running fast and far in steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche 1: Purple Bowl, Size 2, natural cause, no involvement.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche 2: Pilsner Piller, Size 2, natural cause, one climber was hit while leading the ice climb. Miraculously, he held on, his partner was unaffected.&nbsp; VERY close call. Parks Canada responded and confirmed this account with the climbers. Photos are available on our facebook page. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche patrols were conducted on the Maligne Road and the Icefields Parkway Saturday. Visibility was excellent and no new avalanches were observed other than a few loose size 1.5-2 out of very steep rocks where snowpack is shallow facetting it to point of no internal cohesion. Trigger likely was solar influenced but not for all.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 loose natural avalanche, solar triggered, size 1.5 observed east of the Roger's Pass summit on a south aspect at 2590m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A helicopter bombing mission on the sunshine road today produced minimal results to size 2, mostly being loose dry avalanches in the facets. The ski hills are reporting ski cutting newly formed soft slabs to size 1 and newly formed cornices.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were seen in the Maligne and Bald Hills area today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A natural avalanche cycle yesterday producing several avalanches to size 2.5 and two to size 3.0 throughout the highway corridor.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">&quot;Frequent Flyer&quot; in the Connaught drainage had also run yesterday, size 2.0 , just reaching the up track.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche 1: Natural trigger, Size 2, across from Vermillion slide path in Kootenay National Park. South aspect. 50m across and approximately 40cm deep. From steep and almost un-skiable terrain. It occurred within the last 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were seen in the Icefields area today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Four avalanches to size 2.0, two size 2.5 and one size 3.0 were down in the highway corridor yesterday. All natural slab avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">No new observations but poor visibility. Suspect sluffing out of steep lee terrain with strong SW winds. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches up to Class 3 running to top of run-out zones observed today. Explosive control on Sunshine Road produced one Class 3 avalanche that buried road 80 cm deep by 15 metres wide</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Visibility was poor today but numerous size 1 loose snow avalanches were observed on steep slopes and in gulleys below tree line.  These avalanches started in the storm snow and seem to step down to ground involving the weak facet snowpack.  No slab avalanche activity has been observed.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread avalanche cycle was observed along the highway corridor yesterday in storm snow.  Avalanches were up to size 3, and many ran into the fans.  Although we received few reports of natural activity in the backcountry, it is likely that most steep paths produced avalanches in the past 24 hours.  Notables include &quot;Frequent Flyer&quot;.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The wide spread natural cycle that happened on Wednesday is over, however storm slabs are still reactive to skier and explosive triggering. Bombing on highway paths on Thursday resulted in half the bombs producing avalanches in the storm snow with average size Class 2</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday's explosive control on low elevation targets released several size 2 slabs and loose snow avalanches. Natural activity was limited. It appears wind still needs to firm up the snow into a slab. A few size 2 naturals were noted releasing out of steep rocky terrain. Some running a fair distance. They started in the storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday produced many avalanches, mostly in the size 2-2.5 range.  These avalanches primarily involved storm snow.  We have had limited observations In the backcountry, however a widespread natural cycle is suspected.  Natural avalanche activity will likely subside today, but human triggering is still likely.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited Visibility continues. Skiers will experience sluffing in steep terrain. Skier triggering is possible on the Jan 5 interface. Forecasters have been making conservative terrain choices while gathering more information about this layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle occurred during the storm on Wednesday. Since then, natural activity has decreased. Given that there has been a significant new load of snow on a variety of weak surfaces, skier triggering is still possible. I'd recommend easing into terrain this weekend, watching for surface slabs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday's explosive control on low elevation targets released several size 2 slabs and loose snow avalanches. Natural activity was limited. Wind needs to firm up the snow into a slab. Fridays patrol was excellent visibility. Only a few size 2 soft slabs were noted from steep terrain. Sluffs up to size 2 out of extreme terrain were more prevelant. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday along the highway corridor we did not observe any new natural avalanches.  However, visibility was poor. Avalanche control on Wednesday triggered numerous avalanches, mainly size 2-2.5. These avalanches primarily involved storm snow.  We have had limited observations In the backcountry, however a widespread natural cycle is suspected.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has decreased and no new avalanches were observed. This being said, the field team observed whumphing and cracking at tree-line elevations where there had been wind during and after the storm. There were slabs buried during the storm, so even though the surface looks fluffy, there may be hidden slabs awaiting on windward slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday's explosive control on low elevation targets released several size 2 slabs and loose snow avalanches. Natural activity has remain limited. No natural activity was noted today; however, forecasters observed pockets of thin windslabs, minor whumphing and cracking, which should be continually assessed as it seems to be getting worse.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday along the highway corridor we did not observe any new natural avalanches. Avalanche control on Wednesday triggered numerous avalanches, mainly size 2-2.5. These avalanches primarily involved storm snow. Few backcountry observations suggest a large natural cycle occurred during the storm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No new activity observed from a flight north over the Divide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday's explosive control on low elevation targets released several size 2 slabs and loose snow avalanches. Natural activity has remain limited since then as cold temperatures locked it down. No new natural activity was noted Saturday; however, we observed pockets of 10-15cm thick windslabs, minor whumphing and cracking. No Sunday patrol.   </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no new avalanches observed since Jan 10th. Avalanche control on Wednesday triggered numerous avalanches, mainly size 2-2.5. These avalanches primarily involved storm snow. Skiers have reported whumphing on steep south aspects where the sun crust is buried. On steep slopes, expect sluffing in the surface snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Tuesday's warm temps will introduce rapid temperature change to a cold snowpack and may lead to a natural cycle and/or touchy slab conditions, as well as increased loose snow avalanches from steep solar aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers accidentally triggered a size 2.5 avalanche while bootpacking up the SE face of Rogers. It failed on facets on the Jan 4 crust, and propagated 30m upslope. It was 35m wide, 300m long with 1-2m deep debris. One person was involved but was uninjured. There have been no new natural avalanches observed since Jan 10th.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several avalanches were observed in the alpine from recent wind loading from the NW. These observations included Mt. Hector, Observation Peak as well as other locations. The avalanches were between size 1.5 and 2. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous size 2 natural soft and hard slab avalanches observed in the alpine and several size 3.  Many of these slides are stepping to ground and running to valley bottom.  Widespread natural loose dry and spindrift avalanches originating from steep rocky terrain at all elevations.  These observations were made in the Columbia Icefield Area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skiers have been triggering avalanches in isolated locations in the alpine and treeline, mostly on steep solar aspects.  The largest of these was a size 2.5 Sa from two days ago, and a size 1.5 from Grizzly Shoulder yesterday.  Isolated natural avalanches have been observed from steep start zones.  Use caution on wind loaded areas on solar aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few surface windslabs have been observed in the past 3 days sizes 2 to 2.5. These have been in steep terrain near ridge crests or below extreme terrain. Cornice failures, wind loading, and sluffs have served as the triggers. No activity has been seen on the Jan 5 persistent slab: its spotty nature and the cold snow have kept things quiet for now.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">During the wind event over the past few days, several size 1.5 - 2 avalanches were noted in the alpine.  One skier triggered a size 1.5 avalanche near sunshine in an open wind affected lee feature below treeline. May see continued sporadic small avalanches tomorrow with strong winds forecasted, although most of the snow has been moved already.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Basal facet avalanches (both slab and loose) have been observed below treeline today.  Yesterday, numerous size 2 and a few size 3 natural soft and hard slab avalanches were observed in the alpine.  Many of these slides are stepping to ground and running to valley bottom.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most reported avalanches have occurred on S and W aspects in the alpine, and are associated with the January 4 sun crust.  Pockets of wind slab have also been observed to fail in specific terrain, mostly on cross loaded features.  Cornices are beginning to fail, causing avalanches to size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">During the wind event over the past few days, several size 1.5 - 2 avalanches have been noted in the alpine. One natural triggered size 2 avalanche near Bow Summit in an open wind-effected lee feature at tree-line. We may see continued sporadic small avalanches tomorrow with strong winds forecasted, although most of the snow has been moved already.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural slab activity to size 2.5 was observed at treeline and alpine elevations where the new wind slabs released on the January 6th surface hoar layer.  Although they did not travel far, they did step down to the basal facets and November rain crust layers.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most reported avalanches have occurred on S and W aspects in the alpine, and are associated with the January 4 sun crust.  Pockets of wind slab have also been observed to fail in specific terrain, mostly on cross loaded features.  Cornices are beginning to fail, causing avalanches to size 2.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several cornice failures have occurred over the last few days.  Some of these have triggered wind slabs up to size 2 in steep terrain.  One steep cross loaded NW facing gully feature released naturally today as a size 2.5 at about 2000m in a thin snow pack area.  Otherwise little natural activity has been observed over the last several days.    </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural activity was observed on a field trip into the backcountry of Yoho NP. Winds were howling once again at ridge-top from Lake Louise and east, but poor visibility prevented decent observations of high alpine start-zones. Widespread wind-effect was noted above tree-line. It may be hard to find good skiing in the alpine until the next storm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the area around Whistler's, numerous full depth natural slab avalanches have been observed on thin, steep, lee slopes in the alpine.  We are seeing wide propagation to size 3 from continued NW wind loading.  These avalanches are running far in paths with steep run outs.    </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent avalanches have occurred on N aspects in the alpine, and are associated with the moderate to high winds.? Pockets of wind slab have also been observed to fail in specific terrain, mostly on cross loaded features.? Cornices are beginning to fail, causing avalanches to size 2.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today.  Winward slopes have been scoured to the bare rocks in many areas East of the divide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday, in the Whistler's area, numerous full depth natural slab avalanches occurred on thin, steep, lee alpine slopes. In the days preceding, we were seeing up to size 3 from wind loading. They were running far in paths with steep run outs. Saturday's patrol no new avalanches were observed on hy 93 as&nbsp; slightly cooler temps helped to stabilize. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers reported triggerable hard windslabs. A size 1 triggered at the top of &quot;Puff Daddy&quot; on a NE aspect at treeline, fractured 5m above a skier. It was 30cm deep and ran 50m. There have been a few large (sz 2-3) natural avalanches observed daily. These have been triggered by windloading and are from paths with lee start zones. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today. However, yesterday, a recreational party triggered a size 2, hard wind slab avalanche on Narao Shoulder, in Yoho National Park around tree line. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday, numerous full depth natural slab avalanches occurred on thin, steep, lee alpine slopes. In the days preceding, we were seeing up to size 3 from wind loading. They ran far in paths with steep run outs. No new avalanches were observed on Saturday. No patrol occurred on Sunday.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skiers have reported triggerable hard windslabs. On Friday, a size 1 triggered at the top of &quot;Puff Daddy&quot; on a NE aspect at treeline, fractured 5m above a skier. It was 30cm deep and ran 50m. There continue to be a few large (sz 2-3) natural avalanches observed daily. These have been triggered by windloading and are from paths with lee start zones. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Class 2 wind slab on north aspect at 2400 m near Bow Summit was triggered by skiers on Monday. A class 1.5 skier triggered wind slab  (north aspect, 2300m) on Observation peak in past 248 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few natural size 1.5-2 avalanches noted Monday on steep unskiable SW alpine terrain but overall activity has subsided. Previous to Saturday, numerous full depth natural slab avalanches occurred on thin, steep, lee alpine slopes up to size 3. They ran far in paths with steep run outs.   </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">3 natural loose size 2.0 avalanches from solar radiation east of Rogers Pass summit</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural slab size 1.5, suspect on Jan 4th layer in Hermit area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity in the last several days.  Wind slabs in steep terrain are the main concern.  Caution in thin snowpack areas for weak facet layers at the bottom of the snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has stopped however wind-slabs in the alpine are proving to be reactive to skier triggering  in some areas.  A Class 2 wind slab on north aspect at 2400 m near Bow Summit was triggered by skiers on Monday. A class 1.5 wind slab  (north aspect, 2300m) was triggered on Observation peak in past three days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed along the Icefields Parkway today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural loose size 1.5 west of the summit on a south aspect</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural activity today. Hard windslabs to size 2 have been skier triggered within the last few days in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed along the Maligne Lake road today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have observed few natural avalanches in the park recently.  These avalanches have been small and triggered by wind deposited snow or solar radiation inputs.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity today except for sloughing out of climbing terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed along Highway 93 from Jasper to the Weeping wall.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the park yesterday, visibility was poor.? We expect small, loose natural avalanche where happening Wednesday evening through the overnight period due to new snow and moderate winds in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the last week.  The new wind slabs formed on Thursday will be susceptible to skier triggering in steep terrain over the next few days.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunshine village saw ski cutting on reloaded bed surfaces today to size 1 in isolated alpine features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed along Highway 93 and Maligne lake road.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A medium natural avalanche cycle occurred early Friday morning.  Many paths along the highway corridor ran size 2-2.5, with a few running to size 3.0.  Deposits were reaching the end of run outs in some events. We have few backcountry observations, but suspect similar avalanches were occurring up all the drainages.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar point releases from steep south-facing slopes in the alpine. Isolated thin soft slabs noted from NE facing convexities in Kootenay near tree-line.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2.5 slab avalanche was observed originating in a cross loaded alpine gully on a Southwesterly aspect at approximately 2800 meters indicating that the sun is gaining strength in the afternoons.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have observed two moderate natural avalanche cycles involving the storm snow on both Friday and Saturday morning. Many paths along the highway corridor ran size 2-2.5, with a few size 3. Deposits were reaching the end of run outs in some events. We suspect similar avalanches were occurring up all the backcountry drainages. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2.5 slab avalanche was observed on Saturday, originating in a cross loaded alpine gully on a Southwesterly aspect at approximately 2800 meters indicating that the sun is gaining strength in the afternoons.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 natural loose size 2.0 to 2.5 avalanches and 1 natural  slab size 2.5 avalanche were observed within the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches activity observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural slab size 2.0 in the highway corridor west of the Rogers Pass summit</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Many loose snow avalanches have been seen out of extreme terrain on North and East aspects over the last few days. Skiers in steep terrain also experience sluffing. These have generally been slow moving but gain considerable mass. It can be particularly difficult to hold an edge on the hard old snow interface as a sluff starts to move.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasters observed a size 2 naturally triggered avalanche on a N aspect around 2300m on the Sunshine road. This avalanche was likely triggered by a cornice fall and likely occurred within the last 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No New Activity Obs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasters observed a size 2 naturally triggered avalanche on a N aspect around 2300m on the Sunshine road in the last 48 hrs. A natural Icefall avalanche ran off the north face of Mt. Stephen today and just covered the train snow shed. A natural 1.5 was observed on the NE slope of Dolomite peak.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Overnight avalanches have been running to the end of their runnouts up to size 3.0.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little activity. Some wind slabs in steep terrain to size 2. One older size 2 slab (48 hrs + ) in Kootenay may have failed on surface hoar down 50.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">25 new avalanches recorded along the highway from early on the 30th.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little activity. Minor point releases on south-facing aspects reported, all in the surface snow. Expect some natural activity from southerly aspects tomorrow afternoon.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large piece of cornice fell down a steep (45 + degree) east facing alpine slope and did not trigger any weakness.  No other avalanches were observed on Friday with patrols of the Parkway, Whistler Creek and Maligne Road.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed one natural avalanche, sz. 2.5 running to end path along the highway corridor yesterday.  Artillery control produced several avalanches running far with large dust component west of the summit. For all of these observation visibility was poor. A small natural avalanche cycle was triggered by strong winds on the 30th.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity observed in the last few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent cornice fall triggered several large slides to size 3 on southerly aspects on Mt Bosworth and Mt Field. Avalanche control today produced several slides to size 2-2.5 on Mt Bosworth. A size 2 skier-triggered avalanche near Katherine Lake (Dolomite Circuit area) was reported from yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday had a couple loose sz 1's at valley bottom Coleman cliffs running to the highway shoulder. This was solar and warm air influenced. On Friday, a large cornice fell on 45+ degree east facing alpine slope and did not trigger any weakness.  No other avalanches were observed on Friday's patrol Parkway, Whistler Creek and Maligne Road. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Warming and solar radiation will possibly produce loose avalanches on solar aspects this afternoon.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed along the highway corridor yesterday. Artillery control on Thursday night produced several avalanches up to size 3, but mostly size 2-2.5, running far some with large dust component west of the summit. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol was conducted on Sunday. Saturday a couple loose valley bottom sz 1's at Colemans onto shoulder of highway from solar heat. Friday, a large cornice failure on a 45 + degree east facing alpine slope did not trigger any weakness. No other avalanches were observed on Friday's patrol Parkway, Whistler Creek and Maligne Road. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 natural slab avalanches size 2.0 to 2.5 east of Rogers Pass summit from two nights ago due to strong winds.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural loose avalanche size 2.0 west of the summit yesterday, solar triggered.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported or observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant slab avalanche activity has not been noted for sometime. The trend appears to be an increased potential for cornice failures, low to mid elevation solar releases, and increased activity on South aspects related to when the sun impacts the terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche observations from yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been observed in the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches in Jasper or signs of instability related to the widespread persistent hard slab above treeline. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday there were 2  natural, size 2.0, slab avalanches east of the Rogers Pass summit and </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural , size 2.5 avalanche west of the summit.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported or observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches in Jasper or signs of instability related to the widespread persistent hard slab above treeline. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large natural avalanche (size 2.5) was observed by skiers in the Connaught drainage yesterday.  It started low on Mt. Cheops (Cheops N. 4) and ran to 1/3 fan.  Avalanches to size 2.5 were also observed in the highway corridor from Mt. MacDonald.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches reported or observed</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche patrols were conducted today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control operations in the park yesterday produced 30+ avalanches on all aspects.  Most of these involved surface soft slabs, running to end path or  the top of the fans.  Two larger avalanches ran to the highway.  There were no recent reports of avalanches in the back country, and permit areas were closed yesterday for control work.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of avalanches up to size 2 have been observed out of extreme terrain in the last 48hrs.  One appears to have been cornice triggered and likely occurred due to daytime warming today.  If the clear weather and mild temperatures continue we will likely see more avalanche activity or cornice failures due to solar heating in the next few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches reported or observed</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed on a patrol of the Maligne Road on Friday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control operations in the park Wednesday produced 30+ avalanches on all aspects.  Most of these involved surface soft slabs, running to end path or  the top of the fans.  Two larger avalanches ran to the highway.  There were no avalanches reported along the TCH yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed on a road patrol of the Icefields Parkway and Maligne Valley.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">3 natural avalanches were observed yesterday along the highway. They were size 2-2.5 from N and E aspects. Skiers in the Asulkan drainage reported an avalanche (suspect size 2) adjacent to the Cleaver in the Asulkan drainage. These avalanches were likely triggered by loading by steady moderate SW winds. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported recently.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a few size 2 avalanches were triggered on southerly aspects during brief periods of sunshine. Skiers triggered size 1.5 slab avalanches on the SE face of 8812. Recent natural avalanches on N and E aspects have been size 2-2.5 and triggered by loading due to steady moderate SW winds.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Today, strong solar will trigger natural avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large cornice triggered a Class 2 slab out of steep east facing terrain on Wapta Peak in past 48 hours. Otherwise no recent avalanche activity observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, there was a widespread avalanche cycle. They were loose avalanches size 1.5 to 2.5, on solar aspects, triggered by strong sunshine. On Saturday, skiers triggered size 1.5 slab avalanches on the SE face of 8812. Recent natural avalanches on N and E aspects have been size 2-2.5 and triggered by loading due to steady moderate SW winds.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The avalanche activity has subsided from the loose snow avalanches we observed in the last 48 hours. A couple of size 1 loose snow avalanches that occurred in the last 24 hours were observed in the Cameron lake area today on a north aspect at treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">From yesterday morning a natural size 3 slab avalanche off of Mt Leda in the Asulkan valley. 2600m, NE aspect wind loaded ridgetop release, possibly cornice triggered, 40-60cm slab avalanche running ~700m.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 size 2 natural slab east of the Rogers Pass summit in the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 1.5 loose avalanches were observed from steeper alpine features in the Little Yoho Valley. No recent avalanches observed up the Icefields Parkway, but large plumes of wind-transported snow observed off ridge crests.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose snow avalanches originating from a reverse loaded ridge top with a south east aspect in the alpine.  The avalanche patrol was from Jasper to Saskatchewan crossing and return indicating that not much is happening. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of new snow and high to extreme S. winds have resulted in an avalanche cycle in the park overnight.  Most of these were from steep terrain in the highway corridor, and it is likely that similar avalanche activity occurred in the backcountry as well.  Avalanches were running to the middle of the fans, and on average were size 2.5 to 3.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations from Yoho included several size 1.5-2 soft slabs in the alpine, failing in the storm snow, up to 60cm thick. Several size 1.5-2 loose avalanches from NE-SE alpine terrain in Kootenay were observed today, along with shooting cracks in the snow near ridge-crests.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, several loose snow avalanches were observed along SE facing alpine ridge lines.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, field teams remotely triggered size 2 avalanches from 100 meters away.  They also reported shooting cracks and wide propagations, even in low angled terrain below treeline.  Backcountry skiers also reported &quot;touchy&quot; conditions up Connaught Creek and MgGill Shoulder (a solar aspect).  This layer is proving to be easily triggered by skiers</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only a couple of cornice triggered sluffs have been observed out of extreme terrain in the last couple days.  Recent wind slabs seem to be bonding well to the underlying surfaces but may be susceptible to skier triggering in very steep or unsupported terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some new cornice fall and thin wind slabs out of very steep terrain. nothing larger than a small size 2.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, several loose snow avalanches were observed along SE facing alpine ridge lines.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Backcountry skiers reported &quot;touchy&quot; conditions up Connaught Creek and Perly Rock on North aspects where slabs were skier triggered  up to size 1.5. This layer is proving to be easily triggered by skiers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today. Recent natural activity has been limited to steep lee terrain and small cornice falls.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche observations due to snow and low clouds on Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been several reports of skiers accidentally triggering avalanches up to size 2 on the most recent surface hoar layer. These have occurred on all aspects and elevations, with the avalanches propagating up to 80m wide and traveling fast and far. Skiers in these areas have reported clues such as cracks shooting up to 80m from their ski tips</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of small slab avalanches (size 1.5) involving the new storm snow were observe Sunday morning on steep NE facing treeline slopes in the Parkers Ridge area.  No other avalanches were observed along the Icefields Parkway.&nbsp; Visibility was excellent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There continue to be human triggered avalanches up to size 2 on the most recent surface hoar layer. These have occurred on all aspects and elevations, with the avalanches propagating up to 300m wide and traveling fast and far. Yesterday, over 25 size 1.5-3 natural avalanches occurred from steep confined avalanche paths triggered by wind loading. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small point release avalanches in the Lake Louise back country today. Not bigger than size 1. Otherwise nothing reported or observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunday in the Icefields, only two small storm snow slab avalanches were noted from steep NE facing rocky treeline slopes. No other avalanches were observed along the Icefields Parkway and visibility was good. Several size 2 avalanches were noted on Sunday in the Whistler creek alpine. No new naturals were noted Monday and visibility was good. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Clouds reduced solar effects yesterday. When the sun did hit slopes, several size 1.5-2 solar triggered avalanches occurred.  There have been human triggered avalanches up to size 2 on the most recent surface hoar layer. These have occurred on all aspects and elevations, with the avalanches propagating up to 300m wide and traveling fast and far.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread Loose Dry avalanches have been seen failing within the storm snow in mainly extreme terrain. Although most of these events could be called surface sluffs one notable event today ran a considerable distance and reached class 2 in size. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the Sunshine back country, two skiers triggered a size 1 point release avalanche on Twin Cairns. The skiers were able to ski off to the side and were not involved.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new naturals were noted Monday and visibility was good. Visibility was excellent for Tuesday's Icefields patrol. Observed only a couple size 1.5 very steep loose avalanches @ 2600m appearing to be solar triggered. One size 2 thin slab was noted at 2700m E aspect on a very steep unsupported feature. They appear to be stopping where angle changes.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the park, avalanches to size 3, including one glide avalanche, were observed along the highway corridor.  One avalanche was observed below lookout col, shallow (30cm), but very wide propagation.  Several loose snow slides were noted on solar aspects.  Near neighbors have reported many avalanches on the Feb. 12 surface hoar layer.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control on Mt. Whymper and Mt. Dennis produced some large 'facet' avalanches. Explosive control was used to drop the cornices above start zones, which subsequently scrapped out the faceted snowpack. However, without a large cornice like scrub brush, avalanches were actually quite hard to trigger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No Wednesday patrol. Tuesday's patrol observed only a couple size 1.5 very steep loose avalanches @ 2600m appearing to be solar triggered. One size 2 thin slab was noted at 2700m E aspect on a very steep unsupported feature. They appear to be stopping where angle changes.  No naturals were noted on Monday and visibility was good.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity is tapering off in the park, however skiers are still able to pop out slabs in the backcountry.&nbsp; It seems that the weak layer we are tracking now requires a specific trigger, such as a cornice fall, a skier, or even a tree bomb.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity reported today.  Avalanche control on Wednesday produced avalanches up to size 3.  Cornices that were triggered provided enough of a rake to entrain all of the facets in the path, running to within 100m of the road on Mt. Whymper (Kootenay) and Mt. Dennis (Yoho).  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday's patrol into Portal creek from Marmot basin revealed no new avalanches. No Patrol on Wednesday. Tuesday observed only a couple size 1.5 very steep loose avalanches @ 2600m appearing to be solar triggered. One size 2 thin slab was noted at 2700m E aspect on a very steep unsupported feature. They appear to be stopping where angle changes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Few natural avalanches have been observed in the backcountry.  Avalanche control yesterday produced a few avalanches to size 2.5.  While avalanche activity has tapered off lately, test results in profiles consistently produce easy fast shears (RB2 Whole Block) done 50 cm on the Feb. 12 surface hoar PWL.&nbsp; This PWL can be found almost everywhere.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was observed on Thursday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity reported today.   Avalanche control on Wednesday produced avalanches up to size 3.  Cornices that were triggered provided enough of a rake to entrain all of the facets in the path, running to within 100m of the road on Mt. Whymper (Kootenay) and Mt. Dennis (Yoho).  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No Patrol Friday. Thursday's Marmot Basin Portal creek patrol revealed no new avalanches. No Patrol on Wednesday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have not observed any new natural activity in the past few days.  There has also been a lack of observation or reports of skier-triggered avalanches on the Feb 12 surface hoar.  Both natural and rider-triggered avalanche activity will increase with the incoming storm today.  Avalanche control Wednesday produced a several avalanches to size 2.5.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large sloughing was observed off the Stanley Headwall, likely due to strong winds at ridge-top. Experienced climbers in the area said they were large enough to knock climbers off their intended routes. Point releases from steep terrain were observed further south in Kootenay, all in the recent snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity was noted on Saturday's patrol. Its been a while since significant avalanche activity has been observed. Don't let your guard down as allot of variability exists across the landscape.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier triggered a size 2 avalanche yesterday, 1700m, SE aspect down 35-45cm on surface hoar sitting on a 2-3cm crust. See image </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Parks/Glacier/Images/2013-02-23%20Sz%202%20Sc.jpg" target="_blank"><span class="s_9255B882">here</span></a><span class="s_AA239A9B">.  We observed a small natural avalanche cycle mid-day yesterday.  Avalanches sized 1.5-2.5 were running in the storm snow.  None of these avalanche triggered deeper layers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity was noted on Sunday's patrol. It has been a while since any significant avalanche activity occurred.  However, don't let your guard down since there is a lot of variability in the snowpack across the landscape.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">From yesterday: 5 natural slab avalanches ranging in size 2 to 2.5 east of the Rogers Pass summit.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">From Feb 22: Skier controlled size 2.0 slab avalanche on Mt-Fidelity, 33-40deg, south aspect, down 35-45cm, 1700m, 100m wide, 120m long</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed on a field trip in the Lake Louise backcountry. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity was noted on a patrol from town to Medicine lake in the Maligne valley. Snowfall that was expected overnight on Sunday and then through to Tuesday has been reduced to light snow  flurries. It has been a while since any significant avalanche activity occurred. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday:  A skier remote triggered size 2.0 slab avalanche from 30m away. 2010m, North aspect, 35-40degrees, 42cm deep, 100m wide X 100m long on the Feb 12 SH sz 3-8.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">3 avalanches in the highway corridor size 1.5 to 2.0.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of wind triggered avalanches on NE aspects, size 1-2 out of extreme terrain in the alpine have been observed in the last few days.  No other natural avalanche activity has been observed.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No slab avalanches observed. Loose snow avalanches up to Class 1.5 were observed out of steep terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the area today.  It has been a while since any significant avalanche activity occurred.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday west of Rogers Pass summit produced 4 size 3.0 avalanches and 4 size 2.0-2.5.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">7 natural avalanches size 1.5-2.5 east of the summit.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">From Feb 24: Skier remote size 2.0, from 30m. 2010m, north aspect,  35-40 degrees. 42 cm deep, 100m X 100m on Feb 12 surface hoar size 3-8</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small 0.5 soft slabs were ski cut today in the immediate lee of features. Loose snow avalanches to size 1.5 out of steep terrain was observed yesterday.&nbsp;  For the past several days there have been no significant avalanches observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche patrol along Highway 93 from Jasper to Saskatchewan river crossing and return to Jasper produced no new avalanches observations. Some clouds obscured the upper alpine around the crossing. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent avalanche control west of Rogers Pass summit produced 4, size 3.0 avalanches and 4, size 2.0-2.5.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">One natural avalanche was recorded yesterday, East of the summit, a small size 1.5, from a wind loaded start zone which ran to 2/3 path, on a North aspect. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_C9FCE51A { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 12px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_C9FCE51A">A skier accidental size 2.5 occurred on a steep cross loaded feature in the National Geographics, near Lake Louise, click here for image: http://on.fb.me/15m3Ghd (francais: http://on.fb.me/YL9MWx). It was triggered from the upper circle and the skier got out at the lower circle.  The hard slab was 40-60 cm thick and ran the full length of the path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported on Thursday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the park yesterday. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only a few small natural avalanches out of steep wind loaded terrain over the past few days.  Some solar triggered sluffing on steep South aspects today.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_C9FCE51A { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 12px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_C9FCE51A">A skier accidental with no burial size 2.5 occurred on a steep cross loaded feature in the National Geographics, near Lake Louise Thursday.  The hard slab was 40-60 cm thick and ran the full length of the path.  Sunshine and Lake Louise ski hills reporting only sz.1 ski cuts and naturals out of steep ridgetop terrain, reloading through the day.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Visibility is presently obscured along Highway 93, but one avlanche could be heard around the rampart creek hostel area. At lower elevations up to 1600m numerous loose snow avalanches released along the Highway corridor south of the Columbia Icefields.  The heavy snow and possible rain may produce additional loose avalanches in the valley bottoms. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle is just beginning as the storm hits. Rapid loading by snow and moderate S'ly winds are triggering avalanches. Large natural avalanches to size 3 have been observed along the highway running to valley bottom. Precip rates and wind speeds will increase today; expect natural avalanches to run full path in the backcountry.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet slides up to size 1.5 out of steep terrain below tree line were observed today.  As things continue to warm up over the next 36hours we may see more avalanches as the combination of wind, warm temperatures and new snow and/or rain, over load cornices, wind slabs and surface snow.  As temperatures drop the hazard will also lower.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanches are running on all aspects and elevations up to size 3.5. Storm slabs from the upper start zones are pulling out additional moist slabs and wet avalanches in the lower tracks. Steep slopes in the valley bottoms are failing as wet loose avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Visibility is presently obscured along Highway 93, so no avalanche observations were possible between Jasper and Saskatchewan river crossing. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Rapid loading by snow and moderate southerly winds triggered a widespread natural avalanche cycle yesterday. 35 size 2-2.5 and 20 size 3-3.5 natural avalanches were observed along the highway. In avalanche control yesterday, 97 rounds of artillery were fired with the majority triggering size 2-3.5 avalanches, and one size 4. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread avalanche cycle has been occuring over the last 36 hrs. Avalanches to size three have run on all steep terrain and elevations. The slabs have been more likely to propagate at the treeline elevation.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skies and peaks were mostly obscured today by the weather. Very few natural avalanches were observed between Jasper and Parkers ridge. However, good results were produced by avalanche control up to size 2.5 slabs in the parkers ridge area. These slid on weak layers lower in the snowpack. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity continued yesterday.  15 size 2-3 avalanches were observed along the highway, with moist debris and running well into the avalanche fans. The large avalanche cycle during the storm (see yesterdays bulletin) occurred on the storm interface and Feb 12 layer. None appear to have stepped down to deeper layers. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Explosive control on highway paths in Yoho Park produced only minimal results with little slab propagation. Control work on Sunshine Road produced a Class 3.5 that ran to ground on a slope that previously had not slid this winter. Natural over Cascade waterfall in afternoon with  solar heating.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive control work produced some size 3 soft slabs in the Icefields and Maligne lake alpine areas. They slid on the storm snow interface. A few dusted the highway. Natural activity was limited but a few size 2-3's were noted. Winds still need to slab up the storm snow. Gullies above polar circus were 85% cleaned out with control work.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large avalanche cycle occurred over the weekend. Most avalanche paths along the highway (and likely the backcountry) ran, with size 2-3.5 avalanches running into fans. These were failing on the storm interface and Feb 12 layer. None appear to have stepped down to deeper layers. Several large cornice failures, size 2-2.5, were observed yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few size 2 slabs were seen today that appeared to have been in areas just a bit pressed by North winds. The slabs all looked to have been very soft and may have run in the storm snow or on the March 3 rain crust. All of these events were triggered by light loads: minor sluffs from steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a wide-spread natural cycle up to size 3 (at treeline and above elevations) in the storm snow from previous 72 hours. Several avalanches (up to size 2.5)  observed from past 36 hours along Highway 93 North and South (all in the alpine)</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Monday's explosive control work produced some size 3 soft slabs in the Icefields and Maligne lake alpine areas. They slid on the storm snow interface. A few dusted the highway. Natural activity was limited but a few size 2-3's were noted. Winds still need to slab up the storm snow. Gullies above polar circus were 85% cleaned out with control work.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off, but human triggered avalanches remain likely in specific terrain.  Yesterday, skiers triggered a size 3 avalanche on a west aspect in the alpine.  It failed less than a meter from their skis, and propagated 150 m wide, running to valley bottom.  It likely ran on a sun crust interface. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A field team up the Yoho Valley towards Takakkaw Falls observed several sz 3-3.5 avalanches that had run near the end of the last storm (72+hrs). No new avalanches observed in the last 24 hours, but whumphing/settling observed in wind-affected alpine features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Monday's explosive control work produced some size 3 soft slabs in the Icefields and Maligne lake alpine areas. They slid on the storm snow interface. A few dusted the highway. Gullies above polar circus were 85% cleaned out with control work.  No new slab avalanches were observed or reported today.? </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has decreased however large avalanches are still possible.  We are entering a period of &quot;low probability, high consequence&quot; avalanche behavior, in which the likelihood of triggering is less than it was during the storm, but the chance that a skier can trigger a very large avalanche is still very possible.  See </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Parks/Glacier/Images/20130304%20Sa%20Sz%203%202255%20m%20SW%20asp.JPG" target="_blank"><span class="s_9255B882">photo</span></a><span class="s_AA239A9B">:</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a group of skiers remotely triggered, from 100m away, a size 3 slab near Dolomite Peak. They reported it failed on a S aspect and the crown was up to 2m thick. A field team behind the Lake Louise ski area noted several whumph's along open, tree-line features, and as a result, skied conservatively with little confidence in open slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Monday's explosive control work produced some size 3 soft slabs in the Icefields and Maligne lake areas.  Cool alpine temperatures and cloud cover continues to reduce the amount of solar radiation reaching the snowpack today. This will change towards the weekend with increased temperatures and clear skies resulting in higher avalanche danger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has decreased however large avalanches are still possible. We are entering a period of &quot;low probability, high consequence&quot; avalanche behavior, in which the likelihood of triggering is less than it was during the storm, but the chance that a skier can trigger a very large avalanche is still very possible. See </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Parks/Glacier/Images/20130304%20Sa%20Sz%203%202255%20m%20SW%20asp.JPG" target="_blank"><span class="s_9255B882">photo</span></a><span class="s_AA239A9B">:</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread loose dry avalanches were observed today as the new snow failed in steep terrain. Some of these events reached size 2 and the majority occurred in North and East facing terrain. Earlier in the week, there were a few slabs running on suncrusts  as well as a few soft slabs triggered by sluffs in N and E facing terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wednesday, a group of skiers remotely triggered, from 100m away, a size 3 slab near Dolomite Peak. They reported it failed on a SE aspect and the crown was up to 2m thick. Today, a field team around the Sunshine area noted several whumph's and cracking in the snowpack near wind-effected features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Temperatures today remained below freezing, however, several size 1-2 wet snow avalanches were observed on steep south facing slopes below treeline due to intense solar radiation.  On Saturday, temperatures will approach double digits with high solar radiation, this will result in a High avalanche danger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were recorded in Glacier National Park for the last two days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small loose, wet slides were observed from steep solar aspects this afternoon. Whumphing / settling was also observed along ridge features in shallow snowpack areas east of the Divide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Heli bombing had good results on the settled pockets of storm slabs above the Maligne Road on the Medicine Slabs.  No other activity was noted or reported but expect that a few small solar initiated slides occurred on steep south facing slopes below treeline on Saturday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed in the last 3 days. On a west aspect yesterday, skiers reported moist snow sluffing and snowballing on steep slopes below 1600m. Strong solar today will trigger loose avalanches on solar aspects and likely cause cornice failures, which may step down to deeper layers triggering large slab avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 3 natural cornice triggered avalanche occurred near Wall Lake in the last 24hrs out of steep rocky North facing terrain and stepped down to some deeper layers in the snowpack.  Today numerous loose wet avalanches on steep solar aspects up to size 2 were observed at all elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One new size 2 slab on steep non- skiable rock slabs was seen on an easterly aspect. Of note were two previous size 3 avalanches on the same range that must have occurred earlier in the week directly following the storm. Saturday's heli bombing had good results on the settled pockets of storm slabs above the Maligne Road on the Medicine Slabs.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous solar triggered avalanches to size 2 were observed yesterday. These loose avalanches occurred on all solar aspects, with moist debris at lower elevations. A few crossed the uptrack from confined paths up Connaught. None were observed to step down or trigger slabs. Skiers also reported moist snow sluffing and snowballing on steep slopes. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">With a rising freezing level, strong winds and up to 35cm of snow the avalanche danger will increase on all aspects and all elevations.  Slab avalanches will dominate the  alpine and windy  treeline locations on NE aspects. At lower elevations the number and frequency of moist and wet point release avalanche will increase over the next 2 or 3 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Surface snow sluffing out of steep terrain today up to size 1.5.  The last several days have seen numerous loose wet avalanches on steep solar aspects up to size 2, and loose dry avalanches on steep N aspects up to size 2.  With sun and warm temperatures a couple of cornices have triggered slabs out of extreme terrain in the last week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Ski cutting produced small but far running sloughs in steeper terrain today within the top 15-20cm of snow.  The sloughs ran for approx. 200m.  No other avalanches reported or observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed on a road patrol to the Columbia Icefield area, but visibility was poor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">Yesterday: 1 Natural size 2.0 slab avalanche west of Rogers Pass summit on a south aspect</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are currently in a natural avalanche cycle, and will be for the next 24 hours at least. A field team in Yoho remotely triggered a size 2 slab avalanche while moving through moraines above Takakkaw Falls. They noted that conditions were very touchy and retreated. Below tree-line, numerous loose slides to size 1.5 were observed in Yoho.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Poor visibility and flat light has obscured observations from the alpine but numerous piles of avalanche debris have been observed in runouts along highway 93. This indicates that an avalanche cycle is underway with numerous size 2 or 2.5 avalanches occurring in the alpine. At lower elevations loose point releases of size 1 were observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">A cycle of avalanche activity has begun overnight caused by rapid loading of the 30cm of new snow by the strong to very strong winds. Numerous avalanches have been observed this morning running to valley bottom.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lots of natural activity observed today, especially below tree-line in Yoho. Numerous deep, wet slabs to size 3 were seen failing and running to the valley floor. A party of 3 skiers in the Lake Louise backcountry remotely triggered a size 2 slab avalanche from 100m away, 50-60cm deep, 40m wide, and running 200m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Poor visibility and flat light has obscured observations at treeline and above. The  large snowfall amounts in the past 48 hrs and field tests in the alpine and treeline lead us to believe that avalanche activity is underway at upper elevations, both as point release and slabs. Cold temps in the north  have stopped moist avalanche below treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">A cycle of avalanche activity that began yesterday caused by rapid loading of the new snow by the very strong winds, and rising temperatures, continues today. Numerous avalanches were observed yesterday running to valley bottom.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The past two days have seen a widespread cycle of loose wet avalanches up to size 2 on all aspects and at all elevations.  Several wind slab avalanches up to size 2.5 were also observed out of high N aspects occurring in the last several days and likely cornice triggered. This activity should decrease as temperatures cool over the next few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Still a lot of natural activity observed today, especially below tree-line in Yoho and in steeper, rocky terrain. Loose, moist size 1-1.5's observed below tree-line. Visibility into the alpine was poor once again, but moderate to strong winds were transporting the new snow and likely creating natural avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large natural slab avalanches are occurring on steep alpine slopes as moderate to strong SW winds continue to load lee features.  Avalanche control on the Icefields Parkway yielded good results with slab avalanches scouring to ground.  At treeline, mild temperatures and solar exposure provided the trigger Loose wet slides south of the Icefields.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">A cycle of avalanche activity that began on Wednesday caused by rapid loading of the new snow by the very strong winds, and rising temperatures, continued yesterday. Numerous avalanches were observed yesterday running to valley bottom from artillery fire and natural triggers, with many in the size 3.5 range.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive control at sunshine village produced 2 size 3's releasing on basal facets 1m deep and several size 2's confined to the recent storm snow.  These were 40-60cm deep.  One natural cornice release on Mt. Bosworth caused a size 3 within the storm snow within the last 24 hours.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large natural slab avalanches have run on steep alpine slopes.  Several large cornice failures have been observed in the past 48 hrs.  At treeline and below, mild temperatures and solar exposure provided the trigger for small loose wet slides south of the Icefields.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">Natural avalanche activity tapered off yesterday, following this weeks widespread cycle. During the week, numerous avalanches were observed running to valley bottom with many in the size 3.5 range.  Cracking was reported yesterday when ski cutting steep, supported rolls. A slab avalanche 65cm deep was triggered by loading snow. The debris was 1.5m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread avalanche cycle has been occurring over the last few days. Slabs have been observed to size three failing both with cornice fall, wind and wet conditions. Avalanche control today produced some deep slabs and large cornice falls with several size three avalanches with crowns over 1M thick.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Maligne and Icefields patrolled today with 100% visibility. A few size 3 storm slab avalanches have run on large planar alpine slopes. They appear to be initiating in lower start zones around 2500m. Numerous loose solar sluffs to size 2 noted mainly on SW-NW aspects with a few on East aspects. Natural activity was increasing with solar punch.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_E6FD2046 { font-family: 'Verdana';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_E6FD2046">Yesterday, 1 size 2.5 natural avalanche was observed on a SE aspect at 2000m. During last weeks storm, numerous avalanches were observed running to valley bottom with many in the size 3.5 range. Cracking has been reported when ski cutting steep, supported rolls. A slab avalanche 65cm deep was triggered by loading snow. The debris was 1.5m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread avalanche activity has been observed throughout the forecast district. Deep slabs have been observed in many areas to size three. Large cornice falls, storm slabs and deep slabs are still a concern.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field patrol Parkers ridge N and S sides had no cracking or whumphing however the surface slab is evolving and spotty. No new naturals noted. Sunday's patrol a few size 2.5 storm slab avalanches ran on large planar alpine slopes. They initiated in lower start zones at 2500m. Numerous loose solar sluffs to size 2 noted mainly SW-NW aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several skier triggered avalanches in the Hermit area yesterday to size 1.0. These were low density slabs sliding on a crust down 15cm with surprisingly wide propagation running far and fast.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">7 natural slab avalanches in the highway corridor ranging in size from 2.0 to 2.5</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_A8FEC758 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_A8FEC758">It was possible to see evidence of sluffing during the storm on 120317 now that visibility has improved. Otherwise no new recent avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Tuesday's patrol had 100% visibility. Several recent large avalanches to size 3 noted on large high elevation features on various aspects from the past 24hrs. A number of loose moist avalanches up to size 2 were noted mainly from sun impacted slopes, gullies, and cliffs. All these observed recent avalanches were running relatively far.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous new slab avalanches were noted yesterday, associated with the new storm snow and strong winds, in the alpine and treeline.  Several skier triggered avalanches were triggered in the Hermit area two days ago to size 1.0. These were low density slabs sliding on a crust down 15cm with surprisingly wide propagation running far and fast.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday a size 2.5 was noted in Redoubt bowl (near Lake Louise ski area) with a 400 m wide propagation with a crown 60-80 cm thick. Generally, natural activity has tapered, only a few naturals to size 2 were reported in the area yesterday in steeper alpine lee terrain.  Skier triggering of recently developed slabs remains possible to likely.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A recent helicopter flight revealed that a significant avalanche cycle occurred on N to NE alpine slopes to size 3 and on terrain as low as 25 degrees.  All of these avalanches involved the recent storm snow.  The likely trigger for this cycle was continued wind loading along with an increase in temperature.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous slabs were seen yesterday, mostly in the top 30-40cm.  Skiers on Mt. Sifton yesterday were able to cut a cornice to check the slope, and released a size 2.5-3 avalanche on a south aspect, 40cm deep x 100m wide.  Another size 2.5-3 slab was seen in the Asulkan drainage on Mt. Abbott.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A report of a remote triggered sz.3 in the observation peak area (East of hwy. 93 N) on a SW aspect in the alpine March 20.  It was up to 175cm deep on a basal weakness and was 200m wide. &nbsp; A similar sized slide in the Redoubt area in the Lake Louise backcountry (E of Divide) occurred on the 19th.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No visibility into the alpine for Thursday's patrol. No new naturals were noted TL and below.  A helicopter flight Tuesday revealed a significant avalanche cycle occurred on N to NE alpine slopes to size 3 and on terrain as low as 25 degrees. They involved the recent storm snow and the likely trigger was wind loading combined with warm sunny skies.   </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A small avalanche cycle occurred yesterday, mostly from steep start zones on Mt. MacDonald.  Explosive testing yesterday produced a size 1 avalanche on a north aspect.  Two days ago, skiers on Mt. Sifton  cut a cornice to check the slope, and released a size 2.5-3 avalanche on a south aspect.  See photo: </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Parks/Glacier/Images/20130319%20Grizzly%20Pk%20Na%20S%20asp.jpeg" target="_blank"><span class="s_9255B882">Connaught </span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been a fair amount of loose dry activity out of extreme terrain after last week's major storm but surprisingly little slab activity. Yesterday rain as high as 1900m generated minor loose moist activity at lower elevations. New wind slabs are now forming as winds from the West have increased.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Deep persistent slab avalanches have been occurring on basal facets this week. One such avalanche was remote triggered in the Observation Peak area and was up to 175cm deep. Click </span><a href="https://www.facebook.com/photo.php?fbid=488561221193872&amp;set=a.247814718601858.55140.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">here</span></a><span class="s_AA239A9B"> for another avalanche on Redoubt Mountain (E of divide) from March 19th.  Obs. from Yoho today saw natural slabs up to 2.5 within the recent storm snow in the Alp.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 3 triggered by cornice failure in the afternoon heat, scrubbed to ground, 2m crown, and ran full path occurred yesterday in the Shangrila area. A helicopter flight Tuesday revealed a significant avalanche cycle occurred on N to NE alpine slopes to size 3 and on terrain as low as 25 degrees triggered by wind loading and sunny skies.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed along the highway corridor yesterday in the park.  A small avalanche cycle occurred on Wednesday night, mostly from steep start zones on Mt. MacDonald. Also on Wednesday, explosive testing produced a size 1 avalanche on a north aspect at treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanches have been observed on all aspects every day for the past week, some up to size three. These avalanches are more prevalent east of the divide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new noted on Saturday's Icefield's patrol with good visibility. A size 3 was observed Friday off Indian ridge main peak up Whistler creek. It scrubbed to ground and ran far. Thursday in Shangrila a size 3 occurred. It was triggered by cornice fall in the afternoon heat, scrubbed to ground, 2m crown, and ran full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple loose avalanches up to size 2 were observed along the highway corridor yesterday in the park.  A small avalanche cycle occurred on Wednesday night, mostly from steep start zones on Mt. MacDonald. Also on Wednesday, explosive testing produced a size 1 avalanche on a north aspect at treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several cornice falls over the past few days have triggered storm slabs up to size three. Remote triggered deep slabs have been reported in eastern areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No Sunday patrol. Nothing new noted on Saturday's Icefield's patrol with good visibility. A size 3 noted on Friday off Indian ridge main peak up Whistler creek scrubbing to ground, cornice fall trigger, and ran far. Thursday in Shangrila a size 3 was triggered by cornice fall in the afternoon heat, scrubbed to ground, 2m crown, and ran full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanches were triggered during sunny breaks yesterday. 7 size 2 to 2.5 avalanches were observed mid day from solar aspects. Many were loose, with moist debris and a few triggered slabs. Very large cornice failures were reported throughout the Selkirks yesterday. One cornice failure was reported to be 120m long and triggered a size 4!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few size 1-2 avalanches have been running out of steep solar aspects with the effects of daytime heating. As recently as 2 days ago cornice falls were triggering deep slabs on easterly aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the Portal and Whistler creek areas today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers triggered a size 2 on a W aspect at 2585m at 2pm. The avalanche failed on surface hoar sitting on a sun crust. The slab was 25cm deep, 100m wide and 120m long. Tragically, one person was fatally buried 1.9m deep. Natural avalanches were triggered on solar aspects and large cornice failures were reported throughout the Selkirks. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little avalanche activity over the last several days.  Some sluffing in very steep terrain.  Cornice failures remain a concern especially with mild daytime temperatures.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 natural  at treeline on a west aspect on Mt. Andromache. This was a deep slab that failed on the basal facets in the afternoon sun today or yesterday (see facebook page for photo).  Another size 2.5 on a NE aspect of Pilot Mtn.  This was in the alpine and may have been triggered by a cornice fall.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose snow avalanches were observed  on steep South through West aspects at all elevations in the Icefields areas. They originate from steep rock bands and gully features where the sun heats the rocks.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few very large avalanches were observed in the Selkirks yesterday.  Most of these were triggered by cornice failures.  One size 3 was observed from MacDonald into the highway corridor - quite impressive.  Skiers triggered an avalanche two days ago on a west aspect, in a thin snowpack area.  It failed on a suncrust with surface hoar on top.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Afternoon loose wet avalanches on solar slopes in Kootenay within last 24hrs up to size 2.  Most started in steep terrain at treeline and below, with adjacent lower angled slopes not running.  A report of a cornice failure on the N couloir of Bow peak yesterday at 10AM sending one skier tumbling down the gully 200ft in the debris with no injuries.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose snow avalanches were observed  on steep South through West aspects at all elevations in the Icefields areas. They originate from steep rock bands and gully features where the sun heats the rocks. Below treeline, where the snowpack is thin, isothermal conditions are developing.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">More very large avalanches were observed in the Selkirks yesterday.  Most of these were triggered by cornice failures.  Near Glacier Park, a size 4.5 slab was reported, triggered by a cornice fall.  Cornice triggered avalanches have increased throughout the area, with warm daytime temperatures.  Moist avalanches were noted at lower elevations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Steep solar point releases this afternoon reported only to size 1.  Alpine temperatures still fairly cool, keeping most solar activity to treeline and below. Limited field observations today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous wet loose avalanches were observed along the Parkway on all solar aspects from treeline to valley bottom.  Slides ranged from 0.5 to large 2 in size.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous moist avalanches were reported yesterday from Asulkan and Connaught, and along the highway corridor.  Most of these are scrubbing the surface snow, but a few are digging into deeper layers.  Cornice triggered avalanches have increased throughout the area, with warm daytime temperatures, some of which broke down to deep PWL's.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural cornice release off Wapta Peak near Mt Field this morning, good size 2 pulling small slab below and creating a large powder cloud. See photo </span><a href="https://www.facebook.com/photo.php?fbid=491864247530236&amp;set=a.247814718601858.55140.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">here.</span></a><span class="s_AA239A9B"> A size 3 slab off a south aspect was noted in the drainage north of Mt Bourgeau. This likely failed on a sun crust, but scrubbed down to ground lower in the runout. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The wet loose avalanche cycle continues on steep solar aspects from treeline to valley bottom beginning by mid-afternoon.  Slides ranged from 0.5 to large 2 in size.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Afternoons have seen small loose avalanche cycles mostly concentration to SE-W asp.  Yesterday after 1300 avalanches were running up to size 2.5, with one notable size 3.0. Most of these are scrubbing the surface snow, but a few are digging into deeper layers.  Cornice triggered avalanches have increased, with warm daytime temperatures.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are into a predictable pattern of daily heating that produces wet loose avalanches especially as the sun exerts it's effect on Solar Slopes.  Several Cornice failures have been observed as a result of this heating as well and these should remain a concern for skiers seeking dry snow on NW to E aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wet afternoon slides have been covering some tracks. Timing is critical. Cornices have been observed falling off as early as 9:00 AM on sun exposed ridges, some of these have triggered deep slabs on the steep/extreme slopes below them.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The wet loose avalanche cycle continues on steep solar aspects from treeline to valley bottom beginning by mid-afternoon.  A large (size 3) slab avalanche on a steep rocky west facing alpine slope ran full path to ground across from the Parker Slabs, likely a solar trigger.  The alpine is waking up on south to west aspects!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Afternoons have seen small loose avalanche cycles mostly concentration to SE-W asp. Most of these are running in the surface snow. Below treeline and shallow exposed terrain with isothermal snow are weak and can be skier triggered. Cornice failures are still possible, recently not many failures have triggered avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A serac fall triggered a size 3.5 slab on the east face of Mt. Lefroy estimated 1. 5 metres thick and 700m wide. Numerous wet sluffs and slabs to size three with afternoon heating.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous wet loose avalanche size 1-2 are occurring from steep solar aspects from  the valley bottom to 2,300m. Several slab avalanche up to size 2.5 have been observed from the alpine. These are  mostly originating below steep rocky terrain. As the snowpack heats up larger events are possible by mid afternoon potentially running full path. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several glide cracks released yesterday (</span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Parks/Glacier/Images/20130329%20Double%20Bench%20Glide%20Release%20sz%202.5.JPG" target="_blank"><span class="s_9255B882">see photo</span></a><span class="s_AA239A9B">'s), resulting in size 2.5-3 avalanches. Solar triggered avalanches started around 11am, on SE-W aspects. Avalanches are now gouging deeper into the snowpack as it warms up. Below treeline and in shallow areas the snow is becoming weak with warming and can be skier triggered. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread spring cycle up to size three has been occurring on solar aspects starting mid afternoons. Deep wet slabs have been coming out in isolated locations on steep solar aspects late in the day., and some slabs have been observed failing at the bottom of the snowpack in shallow snowpack areas.. Cornices have been falling off also.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several glide cracks released yesterday, resulting in size 2.5-3 avalanches. Solar triggered avalanches started around 11am, on S-W aspects. Avalanches are now gouging deeper into the snowpack as it warms up. Below treeline and in shallow areas the snow is becoming weak with warming and can be skier triggered. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some cloud cover and light alpine winds kept things cooler today. Some isothermal loose snow avalanches on steep solar aspects were observed in afternoon. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity will be at its greatest by mid afternoon. During the morning a strong crust sits on the snowpack and prevents natural avalanches. As the crust melts the danger increases. At that time avalanches up to size 2 can be expected. Falling cornices can trigger full snowpack slabs of size 3 from the alpine. Cool temps reduce the danger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 loose natural avalanches from size 1.5 to 2.5 along the highway corridor.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose wet avalanches to size 2.5 on the west face of Mt Mcgill.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> The natural  isothermal cycle we have been seeing the past few days has subsided. However, if the sun comes out we still expect to see natural activity and the potential for skier triggered avalanches in the afternoon when the surface crusts start breaking down. A skier triggered Class 2 slab to ground was reported near Lake Louise today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity will be at its greatest by mid afternoon or during rain events. During the morning a strong crust prevents natural avalanches. As the crust melts the danger increases. At that time avalanches up to size 2 can be expected. Falling cornices can trigger full snowpack slabs of size 3 from the alpine. Cool temps reduce the danger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 natural moist to wet avalanches from size 1.5 to 3.0 along the highway corridor. Many recent glide crack avalanches.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose wet avalanches to size 2.5 in the backcountry on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">With strong solar inputs a daily cycle of superficial LOOSE WET AVALANCHES spread to affect all elevations and aspects earlier this week.  This same heating also caused many CORNICE FAILURES. A few notable slabs were triggered by cornice failures (large loads) in THIN SNOWPACK AREAS where weak snow has developed in the mid and lower snowpack. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Due to overcast skies the natural  isothermal cycle we have been seeing earlier in the week has subsided. However if the sun comes out we still expect to see natural activity in the afternoon when the surface crusts start breaking down. A skier triggered Class 2 slab to ground was reported near Lake Louise on Wednesday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evening rain may see a short lived spike in wet avalanches at lower elevations this evening. The falling temperatures will put a stop to this as the rain transitions to snow. Ridge top winds will produce soft slabs with the new snow and where this happens to fall on an established melt freeze crust bonding will likely be poor, at least initially. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">3 natural moist to wet avalanches from size 1.5 to 2.5 along the highway corridor. Many recent glide crack avalanches.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose wet avalanches to size 3.0 in the backcountry on solar aspects in the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Sunshine Village was reporting very touchy storm slabs in most alpine areas 15-30cm thick. One size 3 natural on Mount Stephen occurred within the last 24 hours on a North aspect.  Due to poor visibility it is unknown how far up the peak it started from. Click </span><a href="https://www.facebook.com/photo.php?fbid=494287573954570&amp;set=a.247814718601858.55140.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">here</span></a><span class="s_AA239A9B"> for a photo.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Today, several loose avalanches were observed with the new snow, from steep rock cliffs.  Alpine and treeline locations were not visible in the icefields area. Steep, Southerly aspects below 1600m are mostly melted out.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few natural avalanches were reported yesterday, from size 2-3. Many recent glide crack avalanches.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose wet avalanches to size 3.0 in the backcountry on solar aspects over the last week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> One size 2 in the alpine on a NE aspect looked to have occurred within the last 24 hours. It appeared to be 60 cm deep but visibility was poor. Failure plane possibly an ice crust formed on March 14. One skier triggered size 2 storm slab on a N aspect in the alpine reported in the Sunshine back country in steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol on Saturday. On Friday, several loose avalanches were observed from steep rock cliffs.  Alpine and treeline locations were not visible. Steep, Southerly aspects below 1600m are mostly melted out.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery avalanche control along the highway corridor yesterday produced numerous size 2-2.5 loose, moist avalanches.  Most of these avalanches stopped mid-path.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">With poor visibility being a factor, we observed a few natural avalanches yesterday, from size 2-3. In the past week many recent glide crack avalanches have released.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Today 3 size 2 avalanches were observed in the Vernillion Slide paths in Kootenay. The recent moist storm snow likely slid on a crust that was formed last week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported on Sunday. On Friday, several loose avalanches were observed from steep rock cliffs. Steep, Southerly aspects below 1600m are mostly melted out. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed loose, moist/wet natural avalanche running in the highway corridor over the last few day. One notable event was a size 3, from a deep slab release at 1700 m. Glide cracks are still failing, up to size 2.5.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery avalanche control along the highway corridor on Friday produced numerous size 2-2.5 loose, moist avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new naturals observed today.  Limited observations by Parks staff</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday, several loose avalanches were observed from steep rock cliffs. Alpine and treeline locations were not visible. Steep, Southerly aspects below 1600m are mostly melted out. Watch for daytime heating breaking the crust down increasing the danger. Heating also promotes cornice failures which may initiate a large slide. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday: Natural size 3.0 slab avalanche, NW aspect, 2600m, off of Youngs Peak Basin, very wide propagation. Skier triggered size 2.0 slab avalanche, NW aspect, 2750m on Youngs Peak Headwall.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">In the highway corridor 3 natural slab avalanches from size 2.5 to 3.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A field team in the White Pyramid area on the 93N remote triggered a small, thin windslab of little consequence in the alpine today.  Reports indicate increased winds were causing numerous loose dry avalanches out of steep alpine terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity has been reported or observed in the past 5 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday: 4 natural slab avalanches, all size 2.0,  east of the Rogers Pass summit on north facing terrain. From 2 days ago, size 3.0 natural slab avalanche in Youngs Peak Basin and a skier triggered size 2.0 off of Youngs Peak Headwall.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a field team in the White Pyramid area on the 93N remote triggered a small, thin windslab of little consequence in the alpine today.  Reports indicate increased winds were causing numerous loose dry avalanches out of steep alpine terrain. We expect a natural avalanche cycle to occur during the peak of the storm tonight.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the Maligne or Icefields areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few isolated avalanches were noted yesterday, and reports of &quot;whumping&quot; by skiers, mostly in the alpine.  Glide cracks and cornices are growing larger, and are failing unpredictably.  Three days ago, a size 3.0 natural slab avalanche in Youngs Peak Basin and a skier remotely triggered size 2.5 - 3 off of Youngs Peak Headwall.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Touchy soft slabs in the Lake Louise area and up highway 93N were reported in the immediate lees of ridgecrests. Slabs were on average 10-15cm thick, but in some cases up to 30cm thick.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several natural slab avalanches observed in past 24 hours in both the Columbia Icefield Area and Maligne Lake district.  Size 2 - 2.5, on lee aspects below ridgelines between 2200-2400m.  Several large cornice failures reported, and some of these did trigger storm slabs on the slopes below to size 2.  Loose dry point releases on steep N terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle occurred late yesterday and over night with the addition of heavy wet storm snow, up to size 3, running to valley bottom. Glide cracks and cornices are growing larger, and are failing unpredictably.  Heavy loading overnight will make things touchy today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today, but several large cornice failures reported in the past 48hrs.  Of note, several of these cornice falls did trigger deep persistent slabs with crown fracture depths of up to 1m, and some were observed to have triggered more recent storm/wind slabs with a depth of 10-40cm.  </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">    </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday we observed a small avalanche cycle in the new snow.  Moist loose avalanches were not reaching the end of their runnouts, but were observed up to size 2.5 along the highway corridor. On Grizzly shoulder, skier triggered size 1 avalanches occurred on steep, S/SW terrain on a crust. Glide cracks and cornices are still unpredictable hazards</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported, but several large cornice failures reported in the past 72hrs.  Several of these cornice falls did trigger deep persistent slabs with crowns up to 1m, and some were observed to initiate more recent storm/wind slabs with a depth of 10-40cm.   </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural slab avalanche, size 2.0, N aspect, 2100m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Minor DRY LOOSE events have been seen on steep N aspects TL and above. Several small LOOSE WET cycles have occurred on solar aspects as new snow is heated over underlying crusts. There is some evidence of CORNICE FAILURES even with the cool temps, the Cornices that remain along ridgelines are sagging and will not take much encouragement to fall. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches have been observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Several cornice failures occurred last week. A few triggered deep persistent slabs with crowns up to 1m and some initiated wind slabs with a depth of 10-40cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations from yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches have been observed or reported in the past 48 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported in the entire jurisdiction. Several cornice failures occurred last week. A few cornice falls did trigger deep persistent slabs with crowns up to 1m and some initiated wind slabs with a depth of 10-40cm. Observations are supporting a relatively stable snowpack but evaluate each slope as local variations exist.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several slab avalanches on large west facing alpine slopes that received the late day sun were observed yesterday evening. A size 2.5 loose avalanche was observed from a south aspect, and 3 size 2 slab avalanches were occurred on north aspects. Skiers reported slow moving sluffs on steep slopes on a north aspect, and moist pinwheels below 1500m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity over the last 72 hours.&nbsp; Areas that do receive significant amounts of snow in the next 24hours will likely have sluffing and wind slab activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small loose snow avalanches observed off cliff features on Mt. Stephen and Crowfoot Peak during the wind event today and yesterday. This activity is mainly a concern for ice climbers. No new slab avalanche activity over the last 4 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">6 natural slab avalanches size 2.0 were observed east of the Rogers Pass summit from Mt Macdonald and Mt Tupper yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle occurred yesterday morning. One size 3.5 occurred from Mt Macdonald on the north aspect. The avalanche triggered a deep slab on the fan.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Numerourous size 2 to 2.5 avalanches throughout the highway corridor</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the last 24 hours, a size 2 avalanche occurred on a NW aspect of Copper Mountain, just west of Banff, at about 2350 m. It started as a point release which then triggered a 80 m wide slab that failed near ground, down 100-150 cm.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large size 3 was observed off a N aspect on Cheops, as well as several size 2 avalanches from SSE aspects in 8812 Bowl. Several size 2 to 2.5 avalanches throughout the highway corridor yesterday, including a size 2.5 from Moccasin Flats that showed good propagation. All appeared to be 30-40cm deep, likely on the Nov 28 surface hoar/crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations due to poor visibility. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity. A full depth size 2 release on a steep planar NW feature at 2400m on Copper Mtn was observed yesterday. Likely northerly winds and cross loading across this slope with the coming of the arctic front were the trigger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. On Tuesday, a group reported easily ski cutting a few pockets of soft windslab in 8812 bowl. Earlier in the week, several large avalanches natural avalanches occurred. They all appeared to be 30-40cm deep, likely on the Nov 28 surface hoar/crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed today on a flight over the main ranges to Lake O'Hara. A full depth size 2.5 release on a steep planar NW feature at 2400m on Copper Mtn was observed 2 days ago. Likely the northerly winds and cross loading across this slope with the coming of the arctic front was the trigger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. On Tuesday, a group reported easily ski cutting a few pockets of soft windslab in 8812 bowl. Earlier in the week, several large avalanches natural avalanches occurred. They all appeared to be 30-40cm deep, likely on the Nov 28 surface hoar/crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sluffng out of very steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol in forecast region in the last 5 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. On Tuesday, a group reported easily ski cutting a few pockets of soft windslab in 8812 bowl. Earlier in the week, several large avalanches natural avalanches occurred. They all appeared to be 30-40cm deep, likely on the Nov 28 surface hoar/crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the last several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Icefield's highway patrol with excellent visibility revealed no new avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the last several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Highway patrol on Saturday with excellent visibility observed no new avalanches. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 loose and 1 slab, both size 2.0&nbsp; natural avalanches, observed east of Rogers Pass summit in the highway corridor. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Debris from one size 2 avalanche observed Monday falling to mid slope from very steep NE terrain on Buchanan Peak with load from strong westerly winds.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the last several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Patrol on Tuesday observed two avalanches 24 hours old. Size 2-2.5 at 2800m crossloaded SE to S aspect feature on what appears to be the Oct raincrust 40-50cm down. Suspect solar trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural avalanche size 1.5 yesterday east of the Rogers Pass summit on Mt Macdonald. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the last several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Patrol on Tuesday observed two avalanches 24 hours old. Size 2-2.5 at 2800m crossloaded SE to S aspect feature on what appears to be the Oct raincrust 40-50cm down. Suspect solar trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 1.5-2.5 slab avalanches were observed from the steep start zones off Mt Tupper and Mt MacDonald yesterday. Sluffing of the low density surface snow was observed in unsupported terrain, steeper than 35 degrees.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity observed in the last several days. Sunshine forecasters reported ski cutting a size 1.5 avalanche in previously worked terrain. It was a 10-15 cm thick storm slab over a wind slab, which stepped down to the basal rain crust or facets. It was on a lee NE facing alpine feature.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Patrol on Tuesday observed two avalanches 24 hours old. Size 2-2.5 at 2800m cross-loaded SE to S aspect feature on what appears to be the Oct raincrust 40-50cm down. Suspect solar trigger. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of size 1.5-2.5 slab avalanches were observed from the steep start zones off Mt MacDonald and Cougar Corner yesterday. Sluffing of the low density surface snow was observed in unsupported terrain, steeper than 35 degrees.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few thin windslabs have been reported by ski hill avalanche teams. in addition, a natural avalanche ran over a climbing party on Polar Circus yesterday in a near miss with no injuries.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Friday's patrol on Highway 93 resulted in no new avalanches observed. However a report from climbers indicated a size 2 slab release on Thursday morning on the middle pitches of polar circus which is a popular ice climb in the area. Strong wind gusts were evident on the climb at the time of the slide indicating snow loading in the gully.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 size 2-2.5 natural slab avalanches were observed from steep terrain off Mt Tupper and Mt MacDonald on the highway corridor. One natural avalanche, size 3 was also observed yesterday from a north aspect, likely triggered by wind loading. Sluffing of the low density surface snow was observed in unsupported terrain, steeper than 35 degrees.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of wind triggered natural avalanches up to size 2 have been reported out of lee aspects on steep alpine terrain in the last 48hrs with one close call reported on Polar Circus on Cirrus Mountain. With the mild temperatures cornices are forming and are quite delicate at this time.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday morning's avalanche patrol on Highway 93 did not observe any new avalanches. However a 3rd hand report from climbers on Thursday indicated a size 2 slab release on the middle pitches of polar circus. This slide likely originated from a slab in the gully feature.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday natural avalanches with large powder components occurred. We observed avalanches up to size 2.5 east of Rogers Pass along the highway corridor. The public observed avalanches off the steep north facing terrain off Cheops. Sluffing of the low density surface snow was observed in unsupported terrain, steeper than 35 degrees.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the last 3 days in the Park, a few windslabs failed during periods of intense loading near ridgelines and in open gully features at or below treeline. In nearby areas there have been reports of both controlled and accidental avalanches involving windslabs in similar terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 natural avalanche slid over the &quot;Heineken Hall&quot; ice climb on Mt Dennis today reaching the bottom of the run out zone. Several size 1 moist sluffs were also observed in the Field area out of steep tree line terrain. One size 2 was observed yesterday on the &quot;Sacre Bleu&quot; ice climb on Mt Rundle. Wind appears to be the trigger in all cases.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 2.5 off Mt. Tangle observed Sunday afternoon on NE aspect in a steep alpine gully at ridgetop. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed a small natural avalanche cycle along the highway corridor yesterday. The majority of the avalanches were size 1.5 to 2.5 from all aspects depositing snow into runnouts. Two size 3.0 avalanches were observed both east and west of Rogers Pass. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunshine Village reported a ski cut size 2 avalanche that started as a 40 cm deep wind slab, then stepped down to the facets at the base of the snowpack (max fracture depth 150 cm). Similarly, Lake Louise avalanche control reported loose snow avalanches acting as a trigger for a deeper size 2 running on the weak facets near the ground. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2 slab was remotely triggered from below by a skier in the Bald hills on Sunday. The debris stopped short of his location. This occurred on a Northeast aspect in the lower alpine. While there is variable snow distribution on the landscape, there is still potential for slab avalanches to occur in isolated terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural cycle and avalanche control are ongoing. Natural avalanches size 2.5 to 3.5 have been occurring from all aspects and running to the end of their runout zones. Several avalanches were reported from skiers up Connaught yesterday, running off of Mt Cheops and to within 20m of the uptrack on the other side of the valley.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent activity has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A fresh size 2.5 was observed above Bourgeau Right Hand Waterfall that ran down to the edge of the cliffs. The crown was blown in beneath the cornice but suspect storm snow snow slab with wind loading as the trigger.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2 slab was remotely triggered from below by a skier in the Bald hills on Sunday. This occurred on a Northeast aspect in the lower alpine. No other avalanches have been reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, widespread natural cycle producing numerous avalanches to size 3.5 in the highway corridor and in the backcountry. Big avalanches in Connaught Creek were reported; Grizzly slide path, frequent flyer, and paths from Cheops are ran large. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery control in the highway corridor yesterday produced many avalanches to size 3.5. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control work today on the Sunshine road produced </span><a href="https://www.facebook.com/media/set/?set=a.589955951054398.1073741839.145133538869977&amp;type=3&amp;uploaded=4" target="_blank"><span class="s_9255B882">large avalanches</span></a><span class="s_AA239A9B"> (size 2.5-3) on 6 of 9 shots. These avalanches appeared to initiate in the storm snow and step down to the October crust.  Similar reports from the Sunshine avalanche control team and a report of a size 2.5 natural near Bow Summit indicate widespread instability.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 1.5 slab occurred today at 1800m on a slope with a primarily Easterly aspect. This was a thin windslab over basal facets and ran to ground. Colder temperatures should lock the snowpack in for the short term. While there is variable snow distribution on the landscape, there is still potential for slab avalanches to occur in isolated terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle continues. Most were initiated in the alpine and at treeline, running well into runouts, but several triggered slabs below treeline. Along the highway, 1 size 3.5, 4 size 3 and 20 size 2 avalanches were observed yesterday. On Monday skiers reported large natural avalanches occurring up the Connaught drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lee slopes with an easterly component are deep enough to produce large avalanches. Windslabs over loose facets may be very touchy still. All aspects are producing shallow releases which may run quickly in gullied terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 slab occurred today at 2500m on a south easterly slope near the Whirlpool drainage. From a distance this,&nbsp; slab looked&nbsp; like a thin windslab over basal facets and ran to ground.&nbsp; While there is variable snow distribution on the landscape, there is still potential for slab avalanches to occur in isolated terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity has tapered off now that the storm is over. A widespread natural avalanche cycle occurred over the past 3 days, with avalanches up to size 3.5 being triggered by rapid loading by snowfall and wind transport. Most were initiated in the alpine and at treeline, running well into runouts, but several triggered slabs below treeline. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today, but we suspect a few more slabs pulling out on steep lee features with the additional loading. Avalanches to size three both natural and explosive triggered have occurred over the last few days some running full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday, a size 1.5 slab occurred at 1800m on an Easterly slope. This was a thin windslab over basal facets and ran to ground. Visibility was reduced to valley bottom on Friday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off, but slabs now sit at depths easily triggered by light-loads, like humanoids. A number of field crews in the Pass yesterday backed off of larger slopes due to the ease in which the slabs were reacting down 70-80cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Today we observed 2 size 3 avalanches on an east facing cross-loaded alpine bowl near Mt. Saskatchewan/Wilson area,  2 size 2.5 on a similar aspect in the Winston Churchill range. All appeared to have been triggered with continued loading and ran on the Oct crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off, but slabs now sit at depths easily triggered by light-loads, like humanoids. A number of field crews in the Pass yesterday backed off of larger slopes due to the ease in which the slabs were reacting down 70-80cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several natural slab avalanches up to size 3 were reported in alpine terrain in Banff and Jasper over the past 36hrs.  All of these were failing on the weak basal facets layers near the ground. A </span><a href="https://www.facebook.com/photo.php?fbid=604073022976024&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">skier remote size 1.5</span></a><span class="s_AA239A9B"> was also reported yesterday on a small steep N facing tree line feature at Bow Summit.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunday observed several size 2's, likely solar initiated, on the crossloaded gullies above Polar Circus on Mt Cirrus. They stopped mid-path. Saturday, we observed 2 size 3 avalanches on east facing cross-loaded alpine bowl near Mt. Saskatchewan/Wilson area, 2 size 2.5 on a similar aspect in the Winston Churchill range. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed 6 natural avalanches yesterday morning along the highway corridor, running in the storm snow with low density HN and moderate winds. The avalanches were mostly size 2-2.5, and deposited snow at the beginning of the runnouts. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol on Monday. Sunday observed several size 2's, likely solar initiated, on cross-loaded gullies above the weeping wall on Mt. Cirrus. They stopped mid-path. Saturday, we observed 2 size 3 avalanches on east facing cross-loaded alpine bowl near Mt. Saskatchewan/Wilson area, 2 size 2.5 on a similar aspect in the Winston Churchill range. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 loose natural avalanches yesterday in the highway corridor from size 1.5 to 2.0.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 was observed yesterday on a N aspect of Mt. Fairview. It was initiated as a wind-induced spindrift avalanche which pulled out a slab that failed near the ground. This is indicative of the widespread basal weakness present in the snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunday observed several size 2's, likely solar initiated, on cross-loaded gullies above the weeping wall on Mt. Cirrus. They stopped mid-path. Saturday, we observed 2 size 3 avalanches on east facing cross-loaded alpine bowl near Mt. Saskatchewan/Wilson area, 2 size 2.5 on a similar aspect in the Winston Churchill range.  </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">11 natural slab avalanches were observed yesterday ranging in size 2.0 to 2.5 in the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One significant wind slab released on the steep wind loaded face above Wall Lake on Saturday.&nbsp; </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 was observed 2 days ago on a N aspect of Mt. Fairview. It was initiated as a wind-induced spindrift avalanche which pulled out a slab that failed near the ground. This is indicative of the widespread basal weakness present in the snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunday observed several size 2's, likely solar initiated, on cross-loaded gullies above the weeping wall on Mt. Cirrus. They stopped mid-path. Saturday, we observed 2 size 3 avalanches on east facing cross-loaded alpine bowl near Mt. Saskatchewan/Wilson area, 2 size 2.5 on a similar aspect in the Winston Churchill range. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural slab avalanches continued occurring yesterday, even after it stopped snowing, triggered by ongoing wind-loading. They occurred from all aspects on both sides of Rogers Pass, from elevations from 2700m to 1800m, and were size 2-2.5. Several ran into the avalanche paths, moving fast and picking up mass at lower elevations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed over the last 24 hrs. Sporadic natural avalanches up to size 2.5 have been occurring this past week on steep slopes with wind loading.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 new natural slab avalanche observed today in the alpine on a Southwest aspect - size 2. Likely ran on basal weakness. Numerous natural slab avalanches to size 2.5 observed in the past week, primarily on cross loaded gully features in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday. Recent avalanche activity has been triggered by wind-loading, with avalanches to size 2.5 running into avalanche fans. As the storm builds, winds are forecast to increase as well. With lots of snow available for transport, wind loading will magnify precipitation rates and natural avalanches are expected.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2 explosive triggered avalanche on a NE alpine feature at Lake Louise slide on the ground. A few natural loose snow avalanches up to size 2 out of very steep rocky alpine terrain were also observed in the Emerald Lake area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 new natural slab avalanche observed today in the alpine on a Southwest aspect - size 2. Likely ran on basal weakness. Numerous natural slab avalanches to size 2.5 observed in the past week, primarily on cross loaded gully features in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent avalanche activity has been triggered by rapid loading by snowfall and wind-loading, with avalanches to size 2.5 running into avalanche fans. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is a pattern emerging in the Lake Louise area where the snowpack is the shallowest. Steep gullies in alpine areas are producing 100cm deep avalanches to ground (up to size 2), with triggering occurring from thin spots where the snowpack is weakest. A ride in these full-depth avalanches would cause serious injury getting raked over the rocks.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Four new natural slab avalanches size 2.5-3 was observed today in the alpine on a West aspect in shallow rocks, and steep unskiable terrain at 2400m running on basal weakness. The avalanches were restricted to small area between Boundary peak and Panther falls where snowfalls were slightly more and the temperature dropped quickly in 2 hours. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> We have observed natural avalanche activity in the highway corridor in the last 24 hrs. Avalanches are running up to size 3.0 in the storm snow and depositing snow in runnouts. On-going artillery avalanche control is producing few results west of the summit, with results up to size 2.0.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small (size 1) soft slab avalanches were observed in the Sunshine Village area today. No larger avalanches were reported or observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday, four slab avalanches size 2.5-3 was observed in the alpine on a West aspect in shallow rocks, and steep unskiable terrain at 2700m running on basal weakness. The avalanches were restricted to a small zone between Boundary peak and Panther falls along the Parkway. Visibility was poor on Sunday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, natural avalanche activity produced slab avalanches to size 2.5 east of the Rogers Pass summit. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control took place yesterday in the western half of the highway corridor yesterday morning producing avalanches from size 2.0 to 3.0 as well as a sympathetic size 3.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural up to Class 2 observed on Mt. Dennis above the Field Ice Climbs. Several loose snow avalanches out of steep terrain in the recent storm snow observed in Emerald lake area</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No highway patrol today. No new activity reported in the last 24 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">4 natural slab avalanches yesterday from size 2.0 to 2.5 in the highway corridor east of the Rogers Pass summit. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the last 12-24 hrs there have been several avalanches. A natural size 3 in alpine S. asp terrain near Lake Louise (National Geographics), a size 2 scrubbed over Pilsner Pillar climb near Field, and a healthy sz 2 on Twin Cairns near Sunshine - all slid to ground. Also, 2 size 2 storm slab slides occurred at the TL elevation, Emerald Lake area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several new slab avalanches were observed on cross loaded features at tree line and above. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 natural size 2.0 slab avalanches yesterday in the highway corridor from steep gully features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little recent activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanches to size 2.5 over the past few days have been reported with mainly the same characteristics, which are wind slabs failing to ground on the basal weaknesses. Two cornice triggered size 2 avalanches were observed on E/SE. facing Healy creek paths. These were new wind slabs which did not step down to ground and were roughly 40-50cm thick.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On December 31, several new slab avalanches were observed on cross loaded features at tree line and above.  A skier accidental size 1.5 slab occurred at treeline on a Northeast aspect in an open slope. The skier went for a short ride and was buried waist deep.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous size 1.5 to 2.5 slab and loose avalanches were observed from steeper start zones in the western portion of the park yesterday. In the eastern portion, several size 2-3 avalanches were observed from steep terrain on Tupper and MacDonald.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanches to size 2.5 over the past few days have been reported with mainly the same characteristics, which are wind slabs failing to ground on the basal weaknesses. In the last 24 hrs, a storm/wind size 2.5 slab on Micheal Pk in Little Yoho area, NE alpine planar slope, had a long propagation of at least 300 m. It slid on an old snow surface.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrol in the northern end of the forecast area observed a sz 1.5 on a steep sw aspect below tree line.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the highway corridor yesterday. Ski operations adjacent to Glacier National park observed a few slab avalanches within the storm snow, less than 30cm in thickness. As the new storm system rolls in, expect natural activity to pick up.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been no activity in the last few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous avalanches to sz. 2.5 stepping to ground were observed in the alpine today on numerous aspects, but a widespread avalanche cycle did not occur (probably due to lack of wind). A size 2 poured over Pilsner Pillar on Mt. Dennis and left of Silk Tassel on Mt. Field. We have been seeing isolated slides like this every day for over a week.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrols in the forecast area observed a size 2 storm slab at TL and sloughing from steep south facing terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control last night produced significant results, with numerous size 3-3.5's from Mount's Tupper and MacDonald. A possible size 4 from Tupper cleared out mature timber and deposited it on the road. Needless to say, this is likely happening in the backcountry as well.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Today a </span><a href="https://www.facebook.com/photo.php?fbid=609390412444285&amp;set=pb.145133538869977.-2207520000.1388876940.&amp;type=3&amp;theater" target="_blank"><span class="s_9255B882">skier accidental size 2</span></a><span class="s_AA239A9B"> occurred in the W Bowl at Lake Louise which then triggered a size 2.5. Both avalanches failed on the basal facets. Yesterday numerous avalanches to size 2.5 stepping down to ground were observed in the alpine on all aspects including a size 2 on Pilsner Pillar, Mt. Dennis and a size 2 left of Silk Tassel, Mt. Field. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrols in the South end of the forecast area observed one size 3 slab that failed on the basal facets and a size 2.5 storm slab at TL. Numerous smaller slabs from cross loaded features and sloughing was also observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday and Friday we observed a large natural avalanche cycle along the highway corridor. Avalanches were up to size 3.5 and reaching the end of the runnout. A notable size 3.5 from Mt. Tupper cleared out mature timber and deposited around 2 m of debris on the road for 125 m. The largest avalanches occurred on SE through SW aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_2823317B { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 13px;color: #000000; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_2823317B">A widespread avalanche cycle is occurring.</span><span class="s_AA239A9B">  We observed too many </span><a href="https://www.facebook.com/#!/photo.php?fbid=609811785735481&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">size 2's </span></a><span class="s_AA239A9B">to mention, but size 2.5 or larger natural, explosive and human triggered avalanches in </span><a href="https://www.facebook.com/#!/photo.php?fbid=609811709068822&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Corral Creek,</span></a><span class="s_AA239A9B"> </span><a href="https://www.facebook.com/#!/photo.php?fbid=609811699068823&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Emerald Lake</span></a><span class="s_AA239A9B">, Mt. Richardson, Numa Creek, Serac Creek and Floe Lake - we responded to two very close calls, and were amazed at the number of avalanches that occurred today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrols in the South end of the forecast area observed numerous size 3 slabs that failed on the basal facets and widespread smaller avalanches to size 2 on all aspects in the alpine involving windslabs and loose dry avalanches.  With recent storm snow plastered to steep terrain, natural loose dry activity is expected with warming temps.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday along the highway corridor, we observed a couple loose, solar triggered avalanches up to size 2. On Thursday/Friday numerous natural and artillery controlled avalanches along the highway corridor occurred. Artificial triggers produced the largest avalanches up to size 3.5. On Mt. Tupper a size 3.5 cleared out mature timber. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The widespread avalanche activity that was reported yesterday has subsided from its peak, although avalanche control today produced avalanches to size 2.5 in a number of locations. Most failures occurred at the ground level in the depth hoar, and human triggering is still likely in many locations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrols in the South end of the forecast area observed numerous size 3 slabs that failed on the basal facets and widespread smaller avalanches to sz 2 on all aspects in the alpine involving windslabs and loose dry avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, 1 natural size 3.0 glide crack release in the highway corridor west of the Rogers Pass summit.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The widespread natural avalanche activity that was reported two days ago has subsided. No natural avalanches have been reported in the past 24 hours, however human triggered avalanches are still possible in many locations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural cycle of avalanches has tapered off now but the lingering basal instability is still very much a factor as evidenced by the numerous avalanches triggered by Marmot ski patrol in their explosive control runs recently.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Few loose avalanches size 1.0 observed in the highway corridor and in the backcountry yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations on a wildlife survey flight Sunday confirmed a widespread cycle of loose dry avalanches to sz 2 throughout the Park. In N and E alpine slopes that were rapidly loaded during the storm these minor slides triggered several examples of deep persistent slabs to sz 2.5 and up to 1.5m deep on steep, planar or unsupported slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche activity triggered by last weeks storm has subsided and no new avalanches have been observed in the last 36 hrs. The potential for triggering still remains likely.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been observed or reported in the past 72 hour. Increased loading with new snow and or wind will renew avalanche activity at treeline and above with full depth releases anticipated.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of size 2-2.5 slabs from high elevation, steep start zones on Mt Tupper were observed yesterday. Riders reported surface sluffing from steeper terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been noted in the last 24 hrs. Whumphing and collapsing on lower angled terrain indicates the potential for skier triggered slides.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Increased loading with new snow and wind forecast for the weekend will renew avalanche activity at treeline and above. Field team noted the debris of 2 sz 2.5 slab avalanches which had released in the last 24 hours on the basal facets at alpine elevations. Control work with large explosives only produced small slides below treeline today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural activity was observed in the park yesterday, and skiers continued to report surface sluffing from steeper terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">While no new avalanche activity has been observed over the past 48hrs, whumphing on lower angled terrain indicates the continued potential for skier triggered slab avalanches on the basal facets.  Expect increased avalanche activity to begin with the arrival of the new snow tonight!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Increased loading with new snow and wind forecast for the weekend will renew avalanche activity.&nbsp; Field teams noted debris of 2 sz 2.5 slab avalanches which had released in the last 48 hours on the basal facets at alpine elevations. Control work with large explosives produced avalanches to size 2 below on Thursday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday there were several natural avalanches observed east of Rogers Pass. They primarily occurred from steep, wind-loaded features. There were 5 size 2-2.5 avalanches from N aspects and one size 2.0 from a S aspect. Skiers reported sluffing in the top 20cm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some continued loose snow avalanche activity on wind loaded slopes as well as one small slab lower down the slope in CV4.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread avalanche activity today up to size 3 including both Bourgeau Left and Right waterfalls over the climbs, Healy Creek, Cascade Mountain, Corral Creek and Eagle Basin. This avalanche activity is forecast to continue on Sunday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very poor visibility precluded avalanche observation however numerous large avalanches were heard through out the day from the Icefields to Sask Xing.  Sluffing of storm snow on steep banks was observed as well as soft slab avalanches to sz 1.5 at treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches were observed along the highway corridor yesterday on all aspects, running in the storm snow. Most avalanches were sized 1.5 to 2.5, with 4 sized 3.0. A field team yesterday triggered a size 1.0 avalanche at 2000m, east aspect. Obs are limited this morning, however it seems that several events have run to valley bottom.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large natural and </span><a href="https://www.facebook.com/#!/photo.php?fbid=612658538784139&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">explosive controlled avalanches</span></a><span class="s_AA239A9B"> continue to occur in many areas, including slopes adjacent to the ski area boundaries. Numerous human triggered avalanches adjacent to the ski areas, including Maintenance Cliffs near Lake Louise and a very close call on </span><a href="https://www.facebook.com/#!/photo.php?fbid=612658492117477&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Wawa Ridge</span></a><span class="s_AA239A9B">. Avoid all avalanche starting zones on Monday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Control work in the Icefields area produced significant results up to size 2.5. Most slides running in the storm snow but many results continue to scour the ground running on basal facets and burying the road. Of note, in one case, multiple slides were recorded from one shot remotely triggering up to 100m away and over running the road.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have limited observations of a few small natural avalanches up to size 1.5, the occurred overnight. A large cycle of natural avalanche was observed through out the day yesterday. Avalanches were up to size 3.5 depositing snow at the bottom of runnouts. Yesterday, artillery control produced numerous avalanches from all aspects up to size 3.0. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large avalanches to size 3 continue to occur with some running full path. A size 2 in White Rabbit (near Louise ski area) released to ground, causing several sympathetic size 1's. Numerous human triggered avalanches were reported adjacent to ski areas including Ptarmigan Chutes today and Maintenance Cliffs and a close call on </span><a href="https://www.facebook.com/#!/photo.php?fbid=612658492117477&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Wawa Ridge</span></a><span class="s_AA239A9B"> yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A field team in the Maligne Lake area remotely triggered a size 2.5 from a distance of 20m. In the Icefields area a group remotely triggered a size 1.5. Both avalanches were on open slopes at treeline and ran on the basal facet layer. Whumphing and shooting cracks were observed in both locations. Some natural activity to size 2.5 observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle has already begun early this morning setting off large avalanches to size 3.0 in the highway corridor more are expected throughout the region as the storm continues and visibility improves.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">During the storm Friday and Saturday avalanches to size 2.5 have been observed from north and east aspects initiated from steep terrain above. Cornice development during this warm storm has been significant.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control produce large avalanches up to size 3.5 in areas that had not been previously controlled this season. Some had enough force to break mature timber. Additionally there was a skier accidental size 2 in west bowl that caught a party of 3, one fully buried however no injuries. The evidence of a large cycle is present, even BTL.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Natural activity was observed at all elevations in the Icefields area today. The alpine had slabs up to size 2.5 on NE through to SE aspects from 2300m to 2700m. Below treeline, small slab avalanches to size 1.5 occurred on steep open slopes. Monday's field team remotely triggered a size 2.5 from a distance of 20m on a SE aspect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread natural cycle yesterday with avalanches running to size 3.5 in the highway corridor.&nbsp; Backcountry operations in the interior reporting similar observations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery control produced numerous size 3.0 to 3.5 avalanches and most notably a size 4.0 off of Mt Green that released down to the glacial ice depositing snow onto the highway.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">During the storm on Friday and through Saturday a small avalanche cycle occurred with one large avalanche of note from the Akamina Ridge area&nbsp; just west of Wall Lake with debris covering the trail to Bennett Pass. Other avalanches from steep north and east terrain were noted but little activity since Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control today on Mt Dennis produced large avalanches up to size 3.5 in areas that had not been previously controlled this season. Additionally, numerous large natural avalanches observed in Kootenay Park and the Lake Louise Backcountry in the last 24h running to the end of historical runouts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural cycle continues in the forecast area with numerous slab avalanches reported today on all aspects in the elevation range of 1900 to 2600m. Of particular note is a size 3 on Kitchener Shoulder, SE aspect at 2400ms running to ground. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. On Monday, a widespread natural cycle occurred with avalanches to size 3.5. A size 3.5 from Dispatchers Bowl traveled 400m down Connaught creek. Artillery control triggered size 3.0 to 3.5 avalanches and a size 4.0 off Mt Green that released down to the glacial ice depositing snow onto the highway.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control today on </span><a href="https://www.facebook.com/ParksMountainSafety#!/photo.php?fbid=614244521958874&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Bourgeau</span></a><span class="s_AA239A9B"> and </span><a href="https://www.facebook.com/ParksMountainSafety#!/photo.php?fbid=614244518625541&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Vermillion </span></a><span class="s_AA239A9B">produced several large avalanches up to size 3.5. Impressive propagations up to 500 m and crowns as deep as 2 m. Some avalanches today and yesterday triggered large sympathetic avalanches on neighboring terrain and on the backside of features being controlled. Touchy! </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Helicopter control work in the Columbia Icefields area today produced numerous large avalanches to size 3 on a variety of aspects in the alpine. Avalanches showed good propagation and released either at the storm snow interface or on basal facets.  Many ran full path and smaller slides were able to step down to deeper instabilities.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanches yesterday were from steep terrain, including a size 3. On Mon, over 62 natural and 47 artillery controlled avalanches occurred along the highway. Most size 2.5-3.5. A size 3.5 natural from Dispatchers Bowl traveled 400m down Connaught creek. Artillery triggered a size 4.0 off Mt Green that failed to glacial ice &amp; ran onto the highway.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday on </span><a href="https://www.facebook.com/ParksMountainSafety#!/photo.php?fbid=614244521958874&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Bourgeau</span></a><span class="s_AA239A9B"> and </span><a href="https://www.facebook.com/ParksMountainSafety#!/photo.php?fbid=614244518625541&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Vermillion </span></a><span class="s_AA239A9B">produced several large avalanches up to size 3.5. Impressive propagations up to 500 m and crowns as deep as 2 m. The avalanche cycle continued today with small to large fresh avalanches reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations today.  The crew at Marmot reported minimal results on their control work, the exception being a size 2.5 on a SE facing Alpine slope on the basal facets.  Yesterday's control work on the Icefields Parkway yielded large avalanches to size 3 on all alpine aspects releasing on either the storm snow interface or on basal facets. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday. Click on https://www.facebook.com/ParksMountainSafety to see images of the latest avalanche cycle this past Monday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There was some avalanche activity associated with the wind and storm slabs over the last few days. Thursday the warm temperatures were starting to cause snowballing out of rocky areas on steep southeast facing slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One notable size 3 occurred in the last 24 hours on a solar alpine feature near Mt. Hector, stepping to ground. Most natural activity has ceased. Evidence of the widespread cycle from the last week is sobering, with many features having gone wall to wall on the basal layers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Visibility was excellent on Saturday. A couple lower elevation solar facing steep gullies slid to size 2 but otherwise, little else noted. Thursday's control work on the Icefields Parkway yielded large avalanches to size 3 on all alpine aspects releasing on either the storm snow interface or on basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday along the highway corridor. Click on </span><a href="https://www.facebook.com/media/set/?set=a.614166525300007.1073741849.145133538869977&amp;type=3" target="_blank"><span class="s_9255B882">https://www.facebook.com/ParksMountainSafety</span></a><span class="s_AA239A9B"> to see images of the latest avalanche cycle this past Monday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observed some small solar triggered moist sluffs to size 1, and and one notable size 3 on a S facing alpine feature near Mt. Hector which stepped down to the ground in the last 48hrs. Most natural activity has ceased. Evidence of the widespread cycle from the last week is sobering, with many features failing wall to wall on the basal weak layers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol today. The team was responding to an avalanche accident in Valemount. Thursday's control work on the Icefields Parkway yielded large avalanches to size 3 on all alpine aspects releasing on either the storm snow interface or on basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday produced several size 1-1.5 avalanches in alpine terrain. 1 size 2 natural avalanche was observed from steep north facing terrain effecting the highway. All of these avalanches were east of Rogers Pass. Click on </span><a href="https://www.facebook.com/media/set/?set=a.614166525300007.1073741849.145133538869977&amp;type=3" target="_blank"><span class="s_9255B882">https://www.facebook.com/ParksMountainSafety</span></a><span class="s_AA239A9B"> to see images of the latest avalanche cycle this past Monday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed in the last 48-hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has tapered off. Thursday's control work on the Icefields Parkway yielded large avalanches to size 3 on all alpine aspects releasing on either the storm snow interface or on basal facets. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity yesterday</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There has been very little avalanche activity observed in the Park in the last week however avalanches associated with the deep persistent slab have been triggered by a few parties in the neighboring regions. Although avalanche activity may decline in this stable period, remember that this problem will be with us for some time to come</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has tapered off. No new avalanches observed or reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has tapered off. No new avalanches observed or reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose surface sluffing to size 1.0 were observed from steeper (&gt;35 degree) slopes on all aspects in the Fidelity area. Along the highway corridor, thin soft slabs to size 2 were noted from steep, N and S-facing, rocky start zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the last 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field patrols observed three size 1.5 to size 2 slabs on solar aspects in the alpine that had released in the last 24 to 48 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1.0 sluffs and soft slabs have been skier triggered from steeper (&gt;35 degree) slopes running on the Jan 22 surface hoar. Along the highway, a few slabs to size 2 continue to be observed daily from steep terrain on all aspects. Small, loose solar triggered avalanches have also been observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There has been very little avalanche activity observed in the Park in the last week. Although avalanche activity may decline in this stable period, remember that this problem will be with us for some time to come</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed on Saturday. Friday's field patrols observed three size 1.5 to size 2 slabs on solar aspects in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 loose natural avalanches east of the Rogers Pass summit size 1.5 to 2.0</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days. Cooler temperatures are minimizing the solar triggered sluffing. The potential still exists for full depth avalanches on the basal facets in specific terrain features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed. We did observe a minor rockfall event on a south aspect rock face on Saturday afternoon; the end result of melting ice and free water on the face. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We had a vague report of a skier triggered avalanche at the entrance to 8812 bowl from Bruins Pass, size 1.5 at 15:30 on Jan 24, with no other details. Numerous loose naturals up to size 2.5 were observed from that afternoon and yesterday throughout the backcountry in the recent storm snow. All originated from steep south and west slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, small loose moist avalanches were observed from steep solar aspects in the alpine. Skiers reported the top 10cm sluffing fast from ski cuts on steep, shaded aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The  6-10 cm of new snow from Sunday morning has resulted in minor sluffing from steep terrain on all aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, small loose moist avalanches were observed from steep solar aspects in the alpine. Skiers reported the top 10cm sluffing fast from ski cuts on steep, shaded aspects, where the winds have not stripped the surface. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Along the road, a few small slabs to size 2 were observed from steep start zones yesterday. In the backcountry, staff was able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field teams observed three size 2 slab avalanches that occurred in the last 12 hours on southerly aspects at treeline. These had been triggered by last nights snow and strong northerly winds redistributing snow onto the existing surface hoar/facet layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. Recently, field teams were able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine. There are also reports of small loose avalanches (sluffs) triggered by skiers in steep terrain on shaded slopes. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few loose dry natural events have occurred in steep and cliffy terrain. Skiers in steep terrain Monday found the recent snow sluffed easily and ran well on the hard Jan 22 surfaces beneath. Buried windslabs also reacted to skiers in a few places failing on the weak facetted snow that fell Jan 22.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed in the past several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. Small loose avalanches (sluffs) have been triggered by skiers in steep terrain. Recently, field teams were able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 natural cornice triggered avalanche on a SE aspect in Yoho occurred within the last 48 hours.&nbsp;  This was a thin slab in extreme terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. Small loose avalanches (sluffs) have been triggered by skiers in steep terrain. Recently, field teams were able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated small pockets of wind slabs up to 20cm deep and small loose avalanches (sluffs) have been triggered by skiers in steep terrain. Recently, field teams were able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">no new avalanche activity observed</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche patrol today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche patrol today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little activity has been observed in the last 5 days with the exception of minor wind generate surface sluffing in very steep terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche patrol down Highway 93 produced several size 1.5 slab avalanches in the alpine on reverse loaded features likely releasing in the past three days. Similar observations were seen in the Maligne valley as well.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Ski-cuts on steeper north aspects yesterday produced fast sluffing to size 1 in the upper 5-15cm of snow. The faceted snow entrained mass and flowed into low angle terrain over 250-300m downhill. While these sluffs were not big enough to bury a person, you would certainly be pushed over by them, disconcerting in &quot;no-fall&quot; zones with cliffs below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche patrol down Highway 93 on Friday observed several size 1.5 slab avalanches in the alpine on reverse loaded features likely from the previous three days. Similar observations were seen in the Maligne valley as well. No patrol occurred on Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Ski-cuts are producing fast sluffing to size 1 in the upper 5-15cm in loose, faceted snow. The faceted snow entrained mass and flowed into low angle terrain over 250-300m downhill. While these sluffs were not big enough to bury a person, you would certainly be pushed over by them, disconcerting in &quot;no-fall&quot; zones with cliffs below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported Sunday. An avalanche patrol down Highway 93 on Friday observed several size 1.5 slab avalanches in the alpine on reverse loaded features likely from the previous three days. Similar observations were seen in the Maligne valley as well. No patrol occurred on Saturday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Ski-cuts are producing fast sluffing to size 1 in the upper 5-15cm in loose, faceted snow. The faceted snow entrained mass and flowed into low angle terrain over 250-300m downhill. While these sluffs were not big enough to bury a person, you would certainly be pushed over by them, disconcerting in &quot;no-fall&quot; zones with cliffs below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Ski-cuts are producing fast sluffing to size 1 in the upper 5-15cm in loose, faceted snow, entraining mass and flowing into low angle terrain over 250-300m downhill. While these sluffs were not big enough to bury a person, you would certainly be pushed over by them.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">1 natural size 2.0 avalanche east of the rogers Pass summit from Mt Macdonald.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread minor wind generated surface sluffing in steep terrain has gouged into some wind affected slopes to release very soft slabs that wind loading has created over the weak surface facets. Skiers in steep terrain will find very easy sluffing 20 to 30 cm deep. All of these events run far on the firm surfaces until they hit lower angle terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several soft windslabs 10-15 cm deep have been ski cut in windloaded areas above treeline. Avalanche activity is expected to increase on Wednesday and Thursday with the additional new snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported for several days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A brief look at the avalanche paths in the highway corridor this morning showed numerous natural avalanches at all elevations running onto the fans. The same can be expected in the backcountry. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural cycle is now occurring with soft slabs to size 2 in the Alpine and on open slopes at Treeline. Skier triggering of slabs is likely right now at all elevations with remote triggering encountered on steep slopes below treeline. With the additional snow and wind in the forecast the size of these events is likely to increase.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A natural cycle was occurring in the alpine, but visibility was poor. Across the region, several soft touchy windslabs 15-30 cm deep (size 1.5) have been ski cut on all aspects above treeline. Propagations were generally 10-40 m. A general observation was small avalanches were running far an fast, up to 700 m in one case in KNP.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported but visibility was minimal. Expecting some direct action storm snow avalanches in the alpine from this new snow plus what's going to accumulate and windload over the next few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Many avalanche paths in the highway corridor this morning showed numerous natural avalanches at all elevations running onto the fans. The same can be expected in the backcountry. Avalanches will be running fast and far, so give avalanche run-out zones a wide berth.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field trip to Kootenay saw numerous naturals at all elevations to size 2.5 occur within the last 24 hrs. Forecasters were able to ski cut size 2`s which were low density slabs along ridgetops on the Jan 30th surface hoar. These were running 100-300m and were on average 30-40cm deep. Smaller slides were observed in other areas with less storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose snow slides observed out of steep terrain in the alpine (size 1.5).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural and artillery-triggered avalanches were observed yesterday from size 2 to 3.5 at all elevations and aspects. These slides were running fast and to the end of their run-out zones. Below tree-line, natural slabs were failing on the Feb 10 surface hoar/crust/facet sandwich and propagating up to 50m across. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread cycle to size 2 occurred Tuesday as the initial storm formed soft slabs over the facets. Remote triggering was observed at this point and should remain a concern for travelers. Natural activity diminished Wednesday, however on Thursday, a forecaster triggered a South slope above a crust: stomping a foot resulted in a sz 2.5 avalanche. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another field trip to Kootenay, forecasters were able to remote trigger several size 2`s on any steep (&gt;35 deg) unsupported terrain features. One was triggered from 300 m away. These were running 100-300m and were on average 30-40cm deep. One natural size 3 observed on a SE aspect, ran about 1000m. Still touchy around sunshine as well. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lots of natural activity along the highway corridor and in the backcountry was observed yesterday. Numerous size 1.5 to 3's were observed, with all failure planes being in the range of 70-90cm deep, and most slides running full path length. Good propagation was noted in the storm slab, as crown-lines zippered across slopes in the start zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control today produced many avalanches, but they were smaller than expected. On the Sunshine Road and Vermillion Slide paths on 93S slab avalanches up to size 2 were controlled with explosives. All of these avalanches were sliding on the Jan 30th surface hoar/facets layers approx 40cm deep. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier accidental at Marmot basin - size 1.5 on steep Easterly aspect below ridge top at 2100m. This slab was formed by recent loading of the new snow in the past 3 days and slid on the crust/facet interface down 40cm. No natural activity observed on road patrol between Jasper and Saskatchewan crossing.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Many natural and artillery triggered avalanches have been observed recently. Some of these occurances have been very large, running to the end of their run out zones. These avalanches are failing in the storm snow or on the Feb 10th weak layer </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier was caught and buried in a significant avalanche today that the party triggered while descending Rowe Peak at around 2300m on NE-E aspect. Our second peak in natural activity occurred Friday with additional loading but diminished today. Long propagations and the potential for remote triggering have created dangerous conditions for travelers</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous avalanches up to size 2 were observed on Mt. Dennis and Mt. Burgess today. (potentially 24 hours old). Additionally, a natural size 2 avalanche was reported on Quartz Ridge near Sunshine Village. A reliable source indicated that it went today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier accidental yesterday at Marmot basin - size 1.5 on steep Easterly aspect below ridge top at 2100m. This slab was formed by recent loading of the new snow in the past 3 days and slid on the crust/facet interface down 40cm. No natural activity observed on road patrol between Jasper and Saskatchewan crossing yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated natural avalanches were observed yesterday up to size 3.0.  Natural avalanche activity is increasing this morning with moderate to strong winds alpine winds.  Yesterday, several artillery controlled avalanches occurred up to size 3.0.  Including Ross Peak avalanche path off Mt.Green which deposited snow onto the fan.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier was caught and buried in an avalanche yesterday that the party triggered while descending Rowe Peak at around 2300m on NE-E aspect. Widespread natural activity is occurring with the continued rapid loading due to strong winds and snow. Long propagations and the potential for remote triggering have created dangerous conditions for travelers</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural and skier triggered avalanches up to size two are being observed at tree-line and alpine elevations throughout the region. A skier remote class 2 was triggered on a SW aspect near tree line in the Emerald Lake vicinity today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalauncher control work on Parker Slabs produced several size 2 soft slab avalanches up to 50cm deep and 50m wide. No natural activity was observed along the Icefields Parkway.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">6 natural size 3.0 slab avalanches yesterday as well as several size 2.0 to 2.5 slab avalanches within the highway corridor. Backcountry observations have been limited but riders can expect to see lots of evidence of recent natural activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier was caught and buried in an avalanche Saturday that the party triggered while descending Rowe Peak at around 2300m on NE-E aspect. Widespread natural activity is occurring with the continued rapid loading due to strong winds and snow. Long propagations and the potential for remote triggering have created dangerous conditions for travelers</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a small cycle was observed today to size 3 as the recent storm snow has started to become a more cohesive slab. Notable events were multiple skiier triggered and explosives controlled avalanches to size 2.5 at the Lake Louise Ski Area and a size 3 natural off Mt. Wapta that buried the Tak Falls road with 1-2m of debris. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday - there was no natural activity observed between Jasper and The Big Bend and only limited results with the Avalauncher at Parkers Ridge (tree line elevation). </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We had a natural avalanche cycle yesterday morning producing 5 size 3.0 slab avalanches east of the Rogers Pass summit and 1 size 3.5 to the west. Numerous size 2.0 to 2.5 avalanches were also observed within the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle seems to have subsided, however many skier triggered wind slabs up to Class 1.5 were reported today. A size 3 natural off of Mt. Wapta was observed yesterday and explosive control work today on the Yoho Highway Paths resulted in several Class 2.5's and one Class 3 all running in the storm snow.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Patrols occurred in Maligne and Icefields Wednesday. Nothing noted in the Icefields. Skiers triggered a size 2 at Maligne area, 35m wide, 60m long, on a NE aspect 38 degree slope just above treeline on the Feb 10 surface hoar/facet layer. Stability tests showed moderate sudden planar/sudden collapse on this layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control overnight produced numerous size 2-3.5's from all aspects, with many slides extending into the end of the run-out zone. The strong S-SW winds overnight likely produced natural activity in open alpine and tree-line elevations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle seems to have subsided, however skier triggered avalanches are still happening regularly. Several skier triggered avalanches (up to class 2) were reported in the Lake Louise on Thursday. Two skier remotes were reported on the moraine approach to Peyto Glacier on Wednesday. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed in the icefields area today. Wednesday's patrol in the Maligne area produced a size 2 slab that was :35m wide, 60m long, on a NE aspect 38 degree slope just above treeline on the Feb 10 surface hoar/facet layer. Stability tests showed moderate sudden planar/sudden collapse on this layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity is tapering off, but field teams experienced plenty of whumphing and cracking while traveling in supported terrain with no overhead hazard. A significant event west of the park saw wind blast from a slide from extreme terrain knock down 150 year-old timber. Things are still remaining touchy, but with higher consequence now.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread natural activity occurred though the week with many large events flattening trees. Most significant paths ran. One sz 3.5 avalanche was confirmed to have stepped down to the November facets and this is suspected to have occurred in some of the many other sz 3 events which ran full path. Impressive propagations and remote triggering seen.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle seems to have subsided, but skier triggered avalanches (up to class 2) were reported in the Lake Louise on Thursday, and two skier remotes were reported on the moraine approach to Peyto Glacier on Wednesday. Avalanche control on Mt. Whymper today produced avalanches to sz 2.5, likely failing on the Feb.10th interface.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday 2 size 3's and 7 size 2-2.5 avalanches were observed along the highway. Many running right to avalanche fans. And on Wednesday, a significant event west of the park saw wind blast from a slide from extreme terrain knock down 150 year-old timber. Less cracking and whumphing is being observed while traveling but the layers remain reactive. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle seems to have subsided, but skier triggered avalanches (up to class 2) were reported in the Lake Louise on Thursday, and two skier remotes were reported on the moraine approach to Peyto Glacier on Wednesday. Avalanche control on Mt. Whymper yesterday produced avalanches to sz 2.5 failing on the Feb.10th interface.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_2823317B { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday a few natural avalanches were observed along the highway corridor size 1.5 to 2. Close neighbours are reporting large skier triggered avalanches up to size 3. Less obvious signs of instability cracking, recent avalanches activity and whumphing are being observed while traveling </span><span class="s_2823317B">but</span><span class="s_AA239A9B"> the buried weak layers remain reactive. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle seems to have subsided, but a skier triggered avalanche (Class 2) was reported in the Lake Louise area today and a skier remote (Class 1.5) was reported in the Helen Lake area yesterday. Lots of evidence of the recent natural cycle on all aspects at treeline and above (up to Class 2.5) failing on the Feb 10th layer.  </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. Visibility was excellent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
.s_2823317B { font-family: 'Arial';font-style: Normal;font-weight: bold;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday a few natural avalanches were observed along the highway corridor size 2.5 to 3. A fresh size 2.5 avalanche was observed yesterday around noon behind the </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/20140222%20Asulkan%20Cabin%20Avalanche.jpg" target="_blank"><span class="s_9255B882">Asulkan Hut</span></a><span class="s_AA239A9B">. Less obvious signs of instability cracking, recent avalanches activity and whumphing are being observed while traveling </span><span class="s_2823317B">but</span><span class="s_AA239A9B"> the buried weak layers remain reactive. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle has subsided but skier triggered slabs remain likely. A skier triggered (Class 1) from yesterday was observed at treeline on the exit out of Purple Bowl in the Lake Louise area. We have also had other skier triggered, skier remote, and natural avalanches up to Class 2 in the last 72 hours on the Feb 10th interface.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. Visibility was excellent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2.0 natural slab avalanche in the highway corridor east of the Rogers Pass summit yesterday . From Saturday a size 2.5 slab avalanche was observed around noon behind the </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/20140222%20Asulkan%20Cabin%20Avalanche.jpg" target="_blank"><span class="s_9255B882">Asulkan Hut</span></a><span class="s_AA239A9B">. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">avalanche activity has tapered off with the clearing and cooling trend</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a major cycle (occurring 72 hours ago) is still visible throughout the forecast region. However, no new avalanches were observed of reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. Visibility was excellent under blue skies.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">6 natural slab avalanches up to size 2.0 occurred in the highway corridor yesterday. From Saturday a size 2.5 slab avalanche was observed around noon behind the </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/20140222%20Asulkan%20Cabin%20Avalanche.jpg" target="_blank"><span class="s_9255B882">Asulkan Hut</span></a><span class="s_AA239A9B">. This could have been remotely triggered or triggered naturally.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural sz. 2 occurred today due to an inversion and strong sun on a SE aspect above the ice climb Bourgeau right. This was 100m wide but did not go over the climb. Smaller slides to sz.1 on solar aspects at all elevations were seen mainly out of steep, rocky terrain. Explosive control on the Sunshine road produced limited results up to sz. 1.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported. Visibility was excellent under blue skies. Solar radiation may trigger avalanches which are unanticipated by shivering ice climbers below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 2.5 avalanches were observed from southerly tree-line aspects yesterday. From Saturday a size 2.5 slab avalanche was observed around noon behind the </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/20140222%20Asulkan%20Cabin%20Avalanche.jpg" target="_blank"><span class="s_9255B882">Asulkan Hut</span></a><span class="s_AA239A9B">. This could have been remotely triggered or triggered naturally, but is indicative of the lingering persistent weak layer buried a metre below the surface.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous avalanches from size 1.5-2.5 were observed from steep, southerly aspects yesterday along the highway corridor. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off over the last couple of days. Lots of deep fracture lines still visible throughout the park from last week's big cycle. Human accidental and remote triggering of the persistent slab problem continues to be reported in nearby ranges. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported or observed today. Some solar triggered slides up to size 2 occurred in the last several days along with some explosive triggered avalanches up to size 1.5. Whumphing still occuring in lower angled terrain in Kootenay and near Lake Louise over the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One avalanche observed in a open, south facing, cross-loaded gully feature at 2500m on a 35 degree slope. This was likely the result of the current wind transport and overloading of  the facet layer down 50-70cms.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">It's starting to feel like spring. Natural avalanche activity has been occurring from steep solar aspects, producing loose wet avalanches. Numerous size 1.5-2.5 have been observed daily from steep southerly aspects along the highway corridor daily. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported or observed today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. Some previous natural avalanches have been observed in solar aspects below tree line and in cross-loaded lee features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have observed solar triggered natural avalanche activity occurring from steep solar aspects, producing loose wet avalanches in the afternoon when the sun remains out. Numerous size 1.5-2.5 have been observed daily from steep southerly aspects along the highway corridor daily. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported or observed today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday along the highway corridor. Strong solar radiation this past week had produced numerous avalanches up to size 2.5. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size </span><a href="https://www.facebook.com/photo.php?fbid=633391103377549&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">1.5 skier accidental</span></a><span class="s_AA239A9B"> was reported yesterday on an E aspect at 2350m near Bow Summit which failed on the Feb 10th layer. Some natural loose snow avalanches up to size 1, and a small wind slab triggered with explosives were also reported today.  We expect to see a gradual increase in avalanche activity over the next few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanches are starting to run within the highway corridor this morning with this new load. 2 east of the Rogers Pass summit, size 2.5 and 3.0 on a north aspect and one to the west on a south aspect size 1.5. All were steep gully features. Backcountry users can expect to see natural activity increase as it continues to snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One significant persistent slab released just before the cold snap. A few skier triggered windslabs have been seen in the neighboring areas. As we emerge from the cold temperatures there is concern for the persistent slabs to become touchy again. Rapid loading from the forecast wind and snow may result in significant avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose avalanches occurred today in steep terrain. Ski hill forecasters reported ski cutting several soft-hard wind slabs to size 1.5. One size </span><a href="https://www.facebook.com/photo.php?fbid=633391103377549&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">1.5 skier accidental</span></a><span class="s_AA239A9B"> was reported on the weekend on an E aspect at 2350m near Bow Summit. It failed on the Feb 10th layer.  Poor visibility today. Activity will increase with snow &amp; wind forecasted.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose dry avalanches to size 1.5 out of steep rocky East facing terrain in the alpine were observed today.  No new slab avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A notable natural cycle occurred early this morning, with avalanches up to size 3 running from steep gully features on all aspects in the alpine. This coincided with a spike in wind speeds. Backcountry users can expect to see natural activity increase as it continues to snow and as winds increase.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous skier controlled winds-slabs 40-60 cm deep up to size 2 reported from Sunshine. Two significant skier triggered avalanches (Class 2 and 2.5) reported at 1700 m (east aspect) in Kootenay. These initiated 50-100 cm down on the Feb 10 interface and propagated up to 100 m. This suggests that the Feb 10 layer may be getting overloaded.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural cycle occurred yesterday and overnight as the temperatures and winds picked up. Avalanches up to size 3 were running from steep gully features on all aspects in the alpine, especially east of Rogers Pass in the highway corridor. Several of the slides ran to the end of their path, deep down in the valley.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We had limited visibility today. Two significant skier triggered avalanches (Class 2 and 2.5) reported at 1700 m (east aspect) in Kootenay yesterday. These initiated 50-100 cm down on the Feb 10 interface and propagated up to 100 m. Less avalanche activity has been observed in the Louise group over the last few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery control yesterday and this morning has produced excellent results, with avalanches to size 3.5 running fast and to the end of their run-outs. Few observations were made in the backcountry, but given the natural activity in the highway corridor, it is safe to say there is a natural avalanche cycle on-going.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A loose wet avalanche occurred on Wednesday during the rain event. Numerous sz 2 avalanches have been reported in this weeks storm snow in the surrounding areas. Rapid loading from the forecast wind and snow on Sunday along with freezing level forecast to reach 2000m may result in significant avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over the past three days there have been several skier triggered size 2-2.5 avalanches on the Feb 10th interface in steep terrain or steep convexities in Kootenay and in the Sunshine area below treeline. Avalanche control on the sunshine road produced results up to size 3. Less avalanche activity has been observed in the Louise group.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several new natural avalanches observed in the Sir Winston Churchill range up to sz 3. They are isolated to cross-loaded gullies and wind-loaded open slopes in the alpine above 2400ms. The slabs appear to be triggered by loose slides from steeper terrain that is overloading the snowpack. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery control over the past few days produced avalanches to size 3.5 running fast and to the end of their run-outs. Adjacent to the park, an avalanche on the Feb 10 PWL was 1.5m deep and up to 200m wide. Reports also indicate that the storm slab is becoming reactive to skier traffic on steep convex features. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread avalanche cycle to size 3 is occurring at all elevations and aspects, with most of the activity centered around treeline and below in the Kootenay, Yoho, Sunshine area. Most of this is occurring on the Feb 10th layer. Some avalanches in the Kootenay region were scrubbing down to the basal facets at treeline and below.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowballing and pinwheels observed at roadside but limited visibility above. Snowline at 1500m, rain below and a highly variable freezing level observed on the parkway today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 2-3 natural avalanches were observed yesterday along the highway corridor. We are expecting a large natural avalanche cycle to occur this weekend with intense precipitation and warm temperatures. Reports indicate that the storm slab is reactive to skier triggering on steep, convex features with remote triggering a possibility. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind and warm temps caused a cornice failure that triggered a deep slab in the Alpine that ran to valley bottom. Moist snow at low elevations failed as slabs both on storm interfaces and the persistent layer with avalanches running near the bottom of their run outs. Loose wet events have occurred with warm temps BTL and on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle to size 3 occurred on all elevations and aspects today. Much of this is occurring on the Feb 10th layer however we also observed storm slab releases and some deep releases to ground. The cooler temperatures over the next several days will slow down the natural cycle, but skier triggering will remain a concern.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One sz 2 loose slide observed on a west aspect from the steep rocks in the Nigel Basin in the Ice fields area. Visibility was sporadic at times and difficult to get a look into the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have the start of an natural avalanche cycle early this morning, which will continue today. Several size 2-3 natural avalanches were observed along the highway corridor as alpine wind speeds pick up. Reports indicate that the storm slab is reactive to skier triggering on steep, convex features with remote triggering a possibility. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle occurred yesterday on all aspects and elevations and continued today with warmer temperatures and solar input. Bombing today in Kootenay produced </span><a href="https://www.facebook.com/photo.php?fbid=636202913096368&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">large, destructive avalanches</span></a><span class="s_AA239A9B"> on 29/32 shots. Additionally, 2 large skiier triggered avalanches on </span><a href="https://www.facebook.com/photo.php?fbid=636205409762785&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">Mt. Fairview</span></a><span class="s_AA239A9B"> and </span><a href="https://www.facebook.com/photo.php?fbid=636202979763028&amp;set=a.589955951054398.1073741839.145133538869977&amp;type=1&amp;theater" target="_blank"><span class="s_9255B882">West bowl </span></a><span class="s_AA239A9B">show how touchy conditions are right now.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several slabs have been observed on lee slopes in the alpine. This seem to have run in the past 24-36 hrs. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Below tree line there has been a number of moist loose snow avalanches on solar aspects. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday's storm produced a widespread natural avalanche cycle to size 3.5 throughout the highway corridor. Avalanches began dry but ended as moist deposits on their fans. Artillery controlled produced impressive avalanches to size 4.0 showing wide propagation. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle occurred in past 48 hours on all aspects and elevations. Two large remotely skier triggered avalanches were reported yesterday in the Lake Louise area. Natural cycle appears to be over but conditions remain very touchy and reactive to skier triggering.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several slabs have been observed on lee slopes in the alpine. Whumphing and shooting cracks seen and felt today at treeline in conservative terrain reacting on the Feb. facet interface. The natural cycle has slowed down but we expect to see avalanche activity increase when the solar effect is strongest. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">From yesterday there was one size 3.0 natural slab avalanche in the highway corridor and some smaller avalanches closer to highway level on steep rock cuts. Operations in the area are reporting many skier accidental and remote avalanches failing in the storm snow or deeper on the buried weak layers. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">With moderate west winds transporting the 5cm overnight snowfall numerous small avalanches were observed by mid day Tuesday. The large cycle from the weekend ended with the overnight cooling and lower daytime temperatures but solar heating with bluebird days is a concern. Avoid slopes below cornices.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some solar activity up to size 2 in the Mount Field area today. We have seen a large natural avalanche cycle up to size 3.5 over the past week, with wide propagations on many different aspects and elevations. Also, skier triggered avalanches including remote triggered slides to size 3 have been occurring frequently in the past few days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several remote triggered avalanches were observed in the Parker Ridge and Hilda Creek area today. These stiff slabs were easily triggered from adjacent slopes. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Two cornice release triggered slabs that stepped down to ground on steep rocky faces in the alpine today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">With the solar input and warm valley temp's we saw plenty of activity from steeper start zones in the highway corridor. Numerous slides from size 2 to 3.5 were observed, with moist debris in the deposits. Nearby operations are reporting many skier accidental and remote avalanches failing in the storm snow or deeper on the buried weak layers. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A sizable cornice released on the south face of Mt. Bourgeau today which didn't pull a slab on the slope below. Solar aspects have been warming up and we've seen loose wet avalanches out of steep rocky terrain, but the winds have kept things generally cool. Conditions remain touchy and we are still only just coming out of a </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.youtube.com/watch?v=_qSQia8zRxY&amp;list=PLOe6XX2wBaibEmb1auiJiiK96_YaLdHgs" target="_blank"><span class="s_9255B882">major avalanche cycle</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field team remotely triggered several avalanches in the Parker Ridge and Hilda Creek area yesterday. These stiff slabs were easily triggered from adjacent slopes. Two cornice triggered slabs that stepped down to ground on steep rocky faces in the alpine was also observed yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the highway corridor, several size 1.5 to 3 moist avalanches were observed from solar aspects yesterday, all from tree-line elevations or below. A report of a healthy size 2 slab was observed from the steeper terrain on the east side of Glacier Crest.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity noted today. Yesterday there was still extensive whumpfing on Helen Shoulder which was a thin snowpack with a buried sun crust (E side of divide). We are still only just coming out of a </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.youtube.com/watch?v=_qSQia8zRxY&amp;list=PLOe6XX2wBaibEmb1auiJiiK96_YaLdHgs" target="_blank"><span class="s_9255B882">major avalanche cycle</span></a><span class="s_AA239A9B">.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field team remotely triggered several avalanches in the Parker Ridge and Hilda Creek area on Wednesday. These stiff slabs were easily triggered from adjacent slopes and combined with extensive whumphing highlights the unstable nature of the snow at treeline in certain locations.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a group of ski tourers </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/BLong-8436.jpg" target="_blank"><span class="s_9255B882">remotely triggered a size 2.5</span></a><span class="s_AA239A9B"> avalanche from the thin rocky ridge at 2650. The </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/Grizzly%20Mt%20Sr%20%232.JPG" target="_blank"><span class="s_9255B882">avalanche failed over 30m away on a S aspect</span></a><span class="s_AA239A9B">. It was ~1m deep, likely failing on the Feb 10 PWL, and ran over 400m. With the recent sunshine, numerous natural solar triggered avalanches to size 3 have been occurring daily. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Although natural activity has tapered off, helicopter bombing of the path that hit the Akamina parkway on the weekend produced numerous sz 1.5 as well as a 2.5 that almost hit the road again. The active layer is still the Feb facet layer. Small loose dry avalanches occurred today at higher elevations while loose wet avlanaches occurred below 1700m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche observations today. We are still only just coming out of a </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://www.youtube.com/watch?v=_qSQia8zRxY&amp;list=PLOe6XX2wBaibEmb1auiJiiK96_YaLdHgs" target="_blank"><span class="s_9255B882">major avalanche cycle</span></a><span class="s_AA239A9B" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two ski tourers triggered a size 2.5 which failed on the February 10th facet layer in Whistler Creek yesterday. Of note was that the slide was triggered from a shallow rocky area, stepped down to the basal facet layer and was in a cross wind loaded feature at tree-line. Field teams earlier in the week remotely triggered several slabs at tree-line.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Parks Canada responded to a skier accidental size 3 yesterday with involvement. One person was fully buried and dug out by his companions in approx 15min. The subject was critically injured. It occurred on Helen Shoulder on a SW aspect in a large avalanche path facing 93N. Today, evidence of a widespread cycle up to size 3 was noted in Yoho. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations today due to poor visibility on Highway 93 south. Recent remote and skier accidental avalanches as well as extensive whumphing of the snow pack at tree line and the sub alpine is the biggest concern and this problem layer is not likely to heal for the foreseeable future. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural cycle in progress. Avalanches to size 4.0 running to the end of their runouts throughout the highway corridor. The same can be expected in the backcountry.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several new natural avalanches up to size 3 were observed today in the Lake Louise area failing on the Feb 10th layer, as well as a cornice triggered size 2. A skier remote size 3 was triggered today from 800m away on the SW aspect of Mt Daly while descending to Sherbrooke Lake. This was also likely on the Feb 10th layer. Things are still touchy!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field patrols today observed the debris of 3 large avalanches from the weekend cycle. Failure layers appeared to be the February 10th layer on one and the basal facets on the other two larger slides which had been triggered by cornice collapse.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche cycle yesterday and artillery control produced avalanches to size 4.0 with numerous size 3-3.5 within the highway corridor. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">From March 13th, skiers remotely triggered this </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://avalancheinfo.net/Images/Grizzly%20Mt%20Sr%20%232.JPG" target="_blank"><span class="s_9255B882">avalanche on Grizzly peak</span></a><span class="s_AA239A9B">. Note the shallow, south facing start zone. It ran presumably on the March 2nd crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Not much avalanche activity has been seen Sun/Mon because of poor visibility. A long audible avalanche was heard off the back of Cameron Lake on Mon. This was likely the storm snow running on the Mar 14 melt freeze crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field patrols in the past few days observed the debris from numerous large avalanches. These avalanches exhibited wide propagation,  were primarily found in big East facing alpine terrain, and several were triggered by cornice fall.  As the wind begins to push the recent snow around, the likelihood of triggering new slabs will increase.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several natural avalanches from size 2.0 to 2.5 within the highway corridor from early yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today. A large sz.3 cornice triggered avalanche was reported yesterday in the Sunshine back country.  This failed on the Feb.10 interface and stepped to ground in thin areas. We have seen sporadic natural activity like this over the last week.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field patrols in the past few days observed the debris from numerous large avalanches. These avalanches exhibited wide propagation, were primarily found in big East facing alpine terrain, and several were triggered by cornice fall. As the wind begins to push the recent snow around, the likelihood of triggering new slabs will increase.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity in the highway corridor eased yesterday with the cloud cover. A report of a size 2 in the Hospital Knob area of Connaught came in yesterday afternoon. It was suspected to have failed on the more recent, shallower crusts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today. A large sz.3 cornice triggered avalanche was reported on Tuesday in the Sunshine back country. This failed on the Feb.10 interface and stepped to ground in thin areas. We have seen sporadic natural activity like this over the last week. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations today in the Marmot area. Patrols in the past few days observed the debris from numerous large avalanches. These avalanches exhibited wide propagation, were primarily found in big East facing alpine terrain, and several were triggered by cornice fall. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity in the highway corridor has tapered off with cloud cover. A size 2 natural avalanche was reported from the Hospital Knob area of Connaught. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose moist activity has diminished with dropping temperatures however loose dry activity can still be expected out of very steep terrain. Skiers at treeline elevations experienced cracking and small slabs failing in wind effected areas: a sign that storm slabs will be active to skier triggering in steep or unsupported terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">There was one size 2.5 explosive controlled avalanche in Lake Louise area, slid to ground, N aspect, previously controlled terrain. One size 1 sluff observed out of steep rocky terrain NW aspect. Watch out for natural activity related to solar heating over the weekend. Earlier this week, there was a cornice triggered size 3 in the Sunshine region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations today with teams in the Cavell area and a patrol to Saskatchewan Crossing.  Several large avalanches were observed earlier this week. These avalanches exhibited wide propagation, were primarily found in big East facing alpine terrain, and several were triggered by cornice fall. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">8 natural avalanches size 2.5 to 3.0 were observed in the east of the Rogers Pass summit highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches observed today. There was one size 2.5 explosive controlled avalanche in the Lake Louise area yesterday which slid to ground on a N aspect in previously controlled terrain . </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations today with observers in the Maligne and a helicopter flight in the Cavell Area. Several large avalanches were observed earlier this week. on the Feb 10th layer.  These avalanches exhibited wide propagation primarily on big East facing alpine terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 3.0 natural slab avalanche, cornice trigger, in Grizzly Bowl yesterday, east aspect, 2500m. A skier accidental from Bruins Ridge, down 20cm, 20-30m wide, east aspect. Skiers reported hearing many whoomphs on the rolling terrain to Little Sifton. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">4 natural avalanches were observed in the highway corridor from size 2.0 to 2.5 yesterday morning.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches observed or reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations yesterday with observers in the Maligne and a helicopter flight in the Cavell Area. Several large avalanches were observed earlier this week. on the Feb 10th layer. These avalanches exhibited wide propagation primarily on big East facing alpine terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches yesterday observed or reported in the park. Recent large deep avalanches, natural and human triggered have shown that there are areas possible to propagate widely.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches observed or reported today in the forecast region. However, a few large skiier triggered avalanches in the Columbias and K-Country over the last couple days have been surprising professionals and indicate that the weak layers still exist and can be triggered by humans in specific areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches yesterday observed or reported in the park yesterday. On Friday a size 3.5 natural avalanche released in Grizzly Bowl, SE asp, ~2600m, presumably from a cornice trigger. These sporadic events keep our guard up.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">During this cold and calm period, Loose Dry Avalanches have been seen out of steep terrain for the last few days. Today, a small cycle of loose wet avalanches occurred with intense solar heating despite relatively cool air temperatures. Temperatures are expected to spike Tuesday with clear skies: expect an increase in avalanche activity to occur.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches observed or reported today in the forecast region. However, a few large skier triggered avalanches in the Columbias and K-Country over the last couple days indicate that the weak layers still exist and can be triggered by humans in specific areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One sz 2 cornice triggered avalanche on a steep east facing rock slab alpine feature observed today in the Winston Churchill region. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday saw numerous solar triggered loose natural avalanches in the highway corridor and in the backcountry to size 3.0. On Sunday Cheops North 4 (above Connaught creek), north aspect, ~2500m ran naturally size 2.0. From Friday in Grizzly Bowl, east aspect, ~2600m, size 3.5 showing wide propagation possibly cornice triggered.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">One skier triggered size 1.5 avalanche near Sunshine in a steep, alpine chute. Minimal observations due to poor visibility.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sluffing from steep east facing rock slab alpine features observed today in the Winston Churchill region. Overall visibility poor above treeline. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday saw several solar-triggered loose natural avalanches in the highway corridor and in the backcountry to size 3.0. From Friday in Grizzly Bowl, east aspect, ~2600m, a size 3.5 avalanche slid, showing wide propagation from a large trigger (cornice).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new slab avalanches observed or reported today, but several loose snow avalanches (sluffs) up to size 2 were noted.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations along the Icefields Parkway however poor visibility conditions existed. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday there were several reported of loose, moist avalanches triggered by skiers. They were easily triggered and entrained snow to size 2.5. They ran fast and and far, and into mature timber. Numerous natural avalanches also occurred from all aspects along highway corridor and in the backcountry. Most were size 2 but some were up to size 3.5. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A significant solar cycle occurred Tuesday with moist snow gouging down to the March Crusts at low elevations to size 2. Loose Dry activity has also been seen with at least one sz 2 running 350m. Skiers today found easy sluffing with the new snow over the 0326 crust in steep terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
.s_69909980 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">A few soft storm slab naturals to size 2 in immediate lees in the alpine, sluffs up to size 2, and 2 days ago - a size 2.5 to ground in a shallow snowpack area in Little Yoho, East facing alpine slope. A couple of </span><a href="https://www.facebook.com/media/set/?set=vb.145133538869977&amp;type=2#!/photo.php?v=643191412397518&amp;set=vb.145133538869977&amp;type=2&amp;theater" target="_blank"><span class="s_69909980">whumphs</span></a><span class="s_1681A555"> today in Purple Bowl and above Elevator shaft (Louise region) on the basal facets that propagated 50-300 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two size 1.5 to 2 avalanches were observed on steep south facing slopes today.&nbsp; One skier accidental size 2.5 slab was reported from Thursday afternoon in the Shangri-La area.&nbsp; </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers reported easily triggering small size 1-1.5 slabs, where the storm snow failed on convexities and unsupported slopes. On Wed, loose moist avalanches triggered by skiers when a bit of sunshine provided a lot of warmth. These avalanches ran fast and and far, into mature timber, with some growing to size 2.5. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">On a flight E of the Lake Louise ski area today, numerous avalanches were observed in alpine areas mainly on E and SE aspects within the last 24-36 hours. These appeared to be either in the recent HST or on a deeper layer, likely the Feb.10th. A skier accidental sz 1-1.5 was also reported in the Lipalians today which went to ground (80cm). </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One skier accidental size 2.5 slab was reported from Thursday afternoon in the Shangri-La area. Road patrols in the Columbia Icefield Area on Saturday reported a size 2.5 storm slab on an East aspect at 2400m and several smaller storm slabs (sz 1) on steep alpine terrain. Solar aspects were shedding in the afternoon when the sun came out.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, skiers reported easily triggering small size 1-1.5 slabs, where the storm snow failed on convexities and unsupported slopes. On Wed, loose moist avalanches triggered by skiers when a bit of sunshine provided a lot of warmth. These avalanches ran fast and and far, into mature timber, with some growing to size 2.5. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_79B9C72D { font-family: 'Calibri';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_79B9C72D">No avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalaunche control work in the Medicine Lake area today produced several size 2.5 slabs which ran to the lower third of the path and numerous loose dry slides to size 2.  Road patrols in the Columbia Icefields area had limited visibility but did report 1 sz 2 natural avalanche on a North aspect at treeline - 50-75cm deep and 50m wide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose moist avalanches yesterday in the hwy corridor, most size 2.0 and on all aspects. A small cycle out of steep extreme terrain is likely happening now from the overnight storm. These avalanches have the potential to step down to weak layers deeper in the snowpack creating much larger slides, which could run to valley bottoms.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
.s_79B9C72D { font-family: 'Calibri';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous avalanches were observed in the last 24-hours. An explosive triggered avalanche (size 3.5) released on the ground on Mt. Field; 2 size 3 natural avalanches on Mt Fairview and Cathedral; a size 2.5 skier triggered avalanche at Sunshine, and another natural size 2.5 in Richardson's Bowl at Lake Louise. It's been a big 24-hours of avalanches.</span><span class="s_79B9C72D" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalauncher control work in the Medicine Lake area yesterday produced several size 2.5 slabs which ran to the lower third of the path and numerous loose dry slides to size 2. Road patrols in the Columbia Icefields area had limited visibility but did report some small slides on solar aspects in the afternoon.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are into a predictable cycle of daily heating that creates loose wet avalanches on solar aspects. The size of these events will vary with the significance of the heating and the depth of the crust that gets broken down by that heating. The slabs to size 2&nbsp; that have been seen indicate a reactive slab exists in open areas on shaded aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive control on Mt Stephen produced avalanches up to size 2 today. Also, on Wapta peak a cornice dropped and produced a size 2 in extreme terrain within the last 36 hours. On a flight through Yoho evidence of a wide spread cycle up to size 3 was observed that likely occurred in the last 3-4 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier accidental sz 2.5 reported from the Shangri-La area today, triggered remotely from a shallow spot and stepped down to ground.  Avalanche control work in the Columbia Icefield area produced mainly storm slabs in the size 2 range and isolated larger avalanches up to size 3 that failed on ground. Widespread natural cycle in the past 24 hours.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday 1 skier controlled avalanche, size 1.5 on an immediate lee feature of a ridge top, Nw asp, 2420m, down 20cm on the March 22 crust, 100m long and 25m wide</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday along the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two new avalanches reported today - a size 2.5 failed on the ground layer from an explosive at the Lake Louise ski area, and a cornice failure on Mt. Rundle triggered an avalanche in the afternoon. Yesterday 4 separate avalanches were reported to have failed on the ground in shallow snowpack areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">As expected, the warm temperatures and high solar input created numerous moist, loose avalanches up to size 2.5 on S and W aspects yesterday, mainly at tree-line or below. On Monday, there was a skier controlled avalanche, size 1.5 on an immediate lee feature of a ridge top, Nw asp, 2420m, down 20cm on the March 22 crust, 100m long and 25m wide.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lake Louise avalanche safety was reporting large whumpfs in shallow alpine areas today.&nbsp; A profile on one of these slopes found very easy compression results on the basal depth hoar.&nbsp; Yesterday a size 2.5 failed on the ground from an explosive at the Lake Louise ski area, and a cornice failure on Mt. Rundle triggered an avalanche in the afternoon. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier accidental sz 2.5 reported from the Shangri-La area earlier in the week, triggered remotely from a shallow spot and stepped down to ground. Avalanche control work in the Columbia Icefield area on monday produced size 2 storm slabs &amp; isolated larger avalanches up to size 3 that failed on ground. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was very little activity observed yesterday, probably due to the cloud cover hanging overhead for most of the day. A size 2 slide was observed from a steep N-facing start-zone west of Rogers Pass.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only superficial loose moist activity has been seen over the last few days however a few significant slabs were triggered by cornice failures associated with wind and warming last weekend. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Everyday for the past week, there have been avalanches, size 2-3 or large whumphs failing on the facets at the base of the snowpack. They were triggered by cornice, explosive, skier, or prolonged periods of sun. These observations were in the Lake Louise, Hwy 93N, and shallow areas in KNP. Several cornice failures to size 2 observed in past 2 days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. A fridge sized chunk of cornice fell on an alpine East facing slope south of the Icefields failed to trigger anything. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was very little activity observed yesterday, due to cooler temps and cloud cover hanging overhead for most of the day. Avalanches have been observed this morning up to size 2.5 from steep North aspects running to 1/4 of the runnout fans.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A recent sz. 2 wind slab on a N aspect was observed in Yoho from the last 24 hours out of steeper terrain. No other avalanches were reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier accidental on wind loaded terrain feature yesterday, size 1.0, Balu pass, south east aspect, ~2050m, down 10-15cm and 20m wide. Natural avalanches were observed yesterday morning east of the Rogers Pass summit mostly from the steep north facing gullies from Mt Macdonald up to size 2.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Superficial loose moist activity has been seen over the last few days as a result of heating. In the last week a few significant slabs were triggered by cornice failures associated with wind and warm conditions. Expect this activity to increase as we move into warmer days.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. Size 2.5 to ground noted yesterday in Icefields area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 size 2.0 natural avalanches east and west of the Rogers Pass summit within the highway corridor.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet sluffs observed in steep terrain on all aspects below 2000m and on solar aspects to ridge tops. Natural cornice failures have occurred in the last 48hrs creating slab avalanches to size 2. Kananaskis had a skier accidental yesterday in a thin snowpack area failing on the basal facets. We expect avalanche activity to increase tomorrow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">2 size 2.0-2.5 natural avalanches east of the Rogers Pass summit within the highway corridor were observed yesterday</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Widespread superficial loose moist activity has been seen over the last few days as a result of heating. On Sunday heating was strong enough that one of these triggered a 40 cm deep slab on an E aspect. Expect this activity to increase Tuesday. On shaded aspects and at higher elevations a few windslabs have been seen following modest new snow input</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cascade Waterfall and Rogans gulley both produced avalanches size three this afternoon. Also, we have a reliable report that many avalanches occurred on Mt. Rundle between Banff and Canmore. All of these slides were due to rapid warming in the afternoon. Additionally, a small wet slide came down to the ditch on the Field Back Road.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Slab and point release avalanches observed Tuesday up to size 2.5 from treeline and below. All events are stepping to ground. Most are being triggered by warm temperatures and rain. One or two of these events started above treeline in areas where strong and extreme winds, from the SW, are developing wind slabs. These to are steeping down to ground.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Plenty of activity overnight, due to the poor freeze overnight. A cornice-triggered size 3 slab pulled out of Grizzly Bowl overnight on a SE aspect. A size 3 slab failed off Avalanche Crest, running into low angle terrain. A glide-crack failed off of a S-facing slope on Cheops, producing a good size 3 that failed to ground, running into the creek.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cascade Waterfall and Rogans gulley both produced size three avalanches to ground yesterday afternoon during the warm up. Several other natural slides to ground in shallow areas have been reported by our nearest neighbors today as well as a few natural cornice failures. These will continue to occur with daytime heating over the next day or two.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Slab avalanches observed Tuesday and Wednesday up to size 2.5 from treeline and low alpine. All events are stepping to ground. Most are being triggered by wind loading with one cornice failure. Strong WSW winds are developing wind slabs. Afternoon warming and solar radiation is producing point and wet slab releases from below treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Yesterdays natural avalanche cycle produced numerous avalanches from all aspects up to size 3.0. This was followed by some activity overnight from before the freezing temperatures up to size 3.0. Yesterdays shoot produced avalanches up to size 2.5 from about 1/2 the shots.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunshine reported one size 2 cornice failure that landed on the slope below and did not trigger a slab - NE aspect. Otherwise no new avalanches reported or observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Slab avalanches observed Tuesday and Wednesday up to size 2.5 from treeline (TL) and the low alpine. All events are stepping to ground. Most are being triggered by wind loading or cornice failure. Strong SW winds are developing wind slabs. Afternoon warming and solar radiation is producing point and wet slab releases from below treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, several natural avalanches from size 1.5-2.5 were noted from solar aspects. These occurred mainly in the afternoon at the warmest time of day. A notable size 3.5 occurred at the peak of the warmth 36 hours ago on a SW aspect, showing that the persistent weak layers are still active once the snowpack warms up enough.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily loose moist activity on all aspects below treeline and to mountain tops on sun exposed aspects has been seen over the last few days. Minimal cooling overnight has kept solar slopes sensitive to daily solar inputs. This activity should diminish with the cooling expected Saturday however solar heating on Sunday will allow the pattern to resume </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small high altitude sloughing in lee areas and small solar releases in exposed aspects were noted.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of slab avalanches to size 2.5 treeline to alpine have occurred in the past 48 hrs.  A large alpine cornice failure on an E aspect slope had limited propagation.&nbsp; Afternoon warming and solar radiation has produced point and wet slab releases from below treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, several natural size 2 avalanches were noted from solar and polar aspects. These occurred mainly in the afternoon at the warmest and windiest time of day. A notable size 3.5 occurred at the peak of the warmth 2 days ago on a SW aspect, showing that the persistent weak layers are still active once the snowpack warms up enough.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose sluffing out of steep terrain today up to size 1. In the past several days we saw numerous slab avalanches on all aspects and elevations up to size 3 failing on basal facets when the temperatures got really warm. Loose wet avalanches and cornice failures were also observed. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose wet and wet slabs occurred on west aspects below treeline late yesterday afternoon from warm temperatures and solar radiation. Sizes ranged from 0.5 to 2.5.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday at midday a small avalanche cycle occurred during a period of intense precipitation. We observed loose wet avalanches up to size 2.0 on solar aspects and two persistent slab releases up to size 3.0. On Thursday night, we observed an impressive glide crack release on a south aspect east of Rogers Pass that produced a size 3.0 avalanche. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose sluffing out of steep terrain today up to size 1. Loose wet avalanches and cornice failures were also observed today on highway 93N. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 1-2 loose avalanches noted Sunday from alpine to below treeline. They only occurred on the steepest solar aspects and stopped where angle eased. A couple cornice failures were noted in the alpine which did not result in any propagation. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterdays solar inputs were not enough to produce any significant activity, today will be a different story with strong direct sun. A few days ago, glide crack release and slab avalanches to size 3.0 were observed. Loose wet slides to size 2.0 on solar aspects were more common and a possible trigger to the slab releases. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small loose snow point release avalanche were observed on south facing terrain in the afternoon.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several size 1-2 loose avalanches noted Sunday from alpine to below treeline. They only occurred on the steepest solar aspects and stopped where angle eased. A couple cornice failures were noted in the alpine which did not result in any propagation. No avalanche observations on monday were reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday the temperatures stayed fairly cool in the alpine, despite the strong presence of the sun. Combined with light wind, this kept the surface crusts not breaking down until later in the afternoon. A small cycle of loose moist avalanches to size 2.0 started around14:00 and there are likely some from yesterday that we have not observed yet.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily loose moist activity on all aspects below treeline and to mountain tops on sun exposed aspects has been seen over the last few days. This activity has been mainly minor with good freezes and well established surface crusts however size 2 avalanches have been recorded and are a reminder that strong solar heating can break down the crusts. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small loose snow point release avalanche were observed on south facing terrain in the afternoon.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche observations over the past 24hrs on Tue with the cooling temperatures and overcast sky. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Despite the warm alpine temperatures yesterday, only a small cycle of loose moist avalanches to size 2.0 on solar aspects was observed. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Although natural avalanche activity has abated, Banff Visitor Safety performed </span><a href="https://www.facebook.com/ParksMountainSafety/photos/a.745152068868118.1073741868.145133538869977/754634094586582/?type=1&amp;theater" target="_blank"><span class="s_9255B882">avalanche control today</span></a><span class="s_AA239A9B"> on the Sunshine access road. Since the end of the storm there have a number of significant natural and explosive results indicating that there remains plenty of potential for human triggering of avalanches that can be large and destructive.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two natural avalanches to size 2 have come down on north aspects in the alpine in the past 12 hours. Snowpack is settling but any increase in temperature and or wind transport could up the hazard again.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche observed</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday produced a size 2.5 avalanche on the Sunshine roads path. This is indicative that triggering is still possible. No observations or reports of avalanches today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed over the past 72hrs. Prior to the cold snap, a widespread avalanche cycle occurred. Large avalanches, with wide propagations, demonstrated the potential of buried weak layers. Some areas have not yet avalanched, for example the Frequent Flyer path up the Connaught Drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity was observed or reported in the Little Yoho region today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity reported, but a natural 2.5 in the Sunshine backcountry yesterday triggered by wind loading shows large natural avalanches are still possible at higher elevations.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over the past few days, several 1.5 to 2 thin slab avalanches on southerly aspects around treeline have been reported in the Maligne area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed over the past 3 days. Prior to the cold snap, a widespread avalanche cycle occurred. Large avalanches, with wide propagations, demonstrated the potential of buried weak layers. Some areas have not yet avalanched, for example the Frequent Flyer path up the Connaught Drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity was observed or reported in the Little Yoho region today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations along the Parkway today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few size 1.5, solar triggered, avalanches were observed yesterday. Prior to the cold snap, a widespread avalanche cycle occurred. Large avalanches, with wide propagations, demonstrated the potential of buried weak layers. Some areas have not yet avalanched, for example the Frequent Flyer path up the Connaught Drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">At least two large avalanches occurred near the end of the recent storm: a size 3 hit Cameron Lake and another large crown was seen above Forum Lake. A fracture line profile on Forum ridge today found the November 28 crust to be the bed surface and we suspect very soft snow at the base of the newly formed slabs was the failure plane. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has not been a great deal of natural activity observed however explosive results were reported from around the ski areas and produced slab avalanches up to size 2.5 with the slab failing on the basal facets and crusts right on the ground. These kinds avalanches are a dirty &amp; rough ride through scree, rocks and trees &amp; are human trigger able.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No patrol on Maligne or Parkway today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday. Prior to the cold snap, a widespread avalanche cycle occurred. Large avalanches, with wide propagations, demonstrated the potential of buried weak layers. Some areas have not yet avalanched, for example the Frequent Flyer path up the Connaught Drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little natural activity has been observed recently however explosive triggered slab avalanches up to size 2.5 were reported yesterday from the ski areas with the slab failing on the basal facets and crusts near the ground. These kinds avalanches would result in a dirty, rough ride through scree, rocks and trees and human triggering is possible.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field teams reported several full depth avalanches to size 2 on South East aspects at approximately 2400m. These occurred in the last 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little natural activity has been observed recently however explosive triggered slab avalanches up to size 2.5 were reported yesterday from the ski areas with the slab failing on the basal facets and crusts near the ground. These kinds avalanches would result in a dirty, rough ride through scree, rocks and trees and human triggering is possible.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier triggering is still high in likelihood particularly coupled with the recent daytime warming. Two size 2 skier accidentals were triggered this afternoon just outside ski area boundaries around </span><a href="https://www.facebook.com/ParksMountainSafety/photos/ms.c.eJwzNzU3NjAwMDc3MzU2NjTXM4fyTYwNLS0tTOB8A0sLMzNTQwDk9gmN.bps.a.745152068868118/757300070986651/?type=1&amp;theater" target="_blank"><span class="s_9255B882">Sunshine</span></a><span class="s_AA239A9B"> and</span><a href="https://www.facebook.com/ParksMountainSafety/photos/ms.c.eJwzNzU3NjAwMDc3MzU2NjTXM4fyTYwNLS0tTOB8A0sLMzNTQwDk9gmN.bps.a.745152068868118/757300077653317/?type=1&amp;theater" target="_blank"><span class="s_9255B882"> Lake Louise back country</span></a><span class="s_AA239A9B">. This reaffirms the weak basal layers persist and remain prone to human triggering so very little has changed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No field patrols today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No field patrols today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small avalanches running to the beginning of runouts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is some small solar activity occurring on steep solar slopes especially around black bodies. It is easy to trigger wind slabs in specific locations. We continue to find further evidence of the widespread cycle on November 28 but have seen no recent activity on these layers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control work today at the Lake Louise Ski area triggered avalanches to size 2 in terrain that had been previously controlled. This demonstrates that the weak layers at the base of the snowpack were not cleaned out in last weeks avalanche cycle and will likely be with us for some time.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Dec 9 - Numerous loose dry slides to size 1.5 on steep solar aspects at treeline elevation (2100m) and up to 2400m. Several thin, soft windslabs to sz 1.5 slid naturally in cross loaded features near ridgetops on Medicine slab. One skier accidental wind slab was reported from Hilda Peak - 30cm deep, 40m wide, running 15m - 2400m, South East aspect.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were recorded in the last 24hrs.&nbsp; Rising temperatures and heavy forecast precipitation will result in a rapidly rising avalanche hazard.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches seen in the Little Yoho region today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Good observations today in Kootenay Park and highway 93 N revealed a distinct lack of avalanche activity. Sunshine ski area reports a similar lack of avalanches. However, the low elevation rainfall resulted in widespread avalanche activity in the ice climbing gullies down in Field (on Mt. Dennis). </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations in the alpine and treeline today due to the poor visibility. Size 2 avalanche had occurred in the last 24 hours at a below treeline location in the Maligne Lake area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity started yesterday, with numerous size 2-2.5 avalanches occurring from all aspects and running onto avalanche fans. By the end of the day avalanche debris was becoming wet in character. Widespread avalanche activity is expected today due to rapid loading by rain and wind.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread avalanche activity was observed at low elevations today in Yoho Park.  Mostly in the ice climbs near Field.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a small cycle in Yoho Park at and below treeline due to Wednesdays warm temperatures and rain. A fresh slab in past 24 hours was observed on the east side of Mt. Victoria. (2900 m, size 2.5, 200m wide, approx 50 cm deep).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two size 2 skier remote slab avalanches reported in the Nigel Basin today on Easterly aspects at treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity continued yesterday, with numerous size 2-2.5 avalanches occurring from all aspects and running onto avalanche fans. Avalanche debris is wet in character. The Laurie avalanche path, on the park's west boundary produced another size 3 avalanche yesterday. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose moist activity has been occurring over the last three days. Most of these events have been out of very steep and rocky terrain. This activity has been a result of the extreme heating and rain that has also created a zero degree snowpack to the ground to an elevation of about 1900m and toppled most of the frozen waterfalls. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a small cycle in Yoho Park at and below treeline due to Wednesdays warm temperatures and rain. A fresh slab in past 24 hours was observed on the east side of Mt. Victoria. (2900 m, size 2.5, 200m wide, approx 50 cm deep).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several avalanches up to sz 2.5 was observed in the field today. Control results at Marmot produced a very large size 3.5 that went full depth wall to wall in Charlie's Bowl!&nbsp; Several other large natural avalanches were also reported around the ski hill on wind loaded alpine slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity continued yesterday within the highway corridor with numerous size 2-3.0 avalanches occurring from all aspects and running onto avalanche fans. Avalanche debris is wet in character. A natural cycle is expected in the backcountry as well but observations are limited at this time.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A road patrol today though Field to Emerald Lake did not see any new avalanche activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few explosive triggered avalanches up to size 2 were observed at Sunshine Village today failing on the basal crust/facet combination. No new natural avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous activity offering interesting results on the November rain crust persistent weak layer. Long delays of a few minutes after an explosive detonation at Marmot Basin released a size 3 that ran much further than expected from a heavily loaded ridge top feature. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control within the highway corridor west of the Rogers Pass summit yesterday produced mainly avalanches size 2.5 and up to size 3.0 showing wide propagation on the Nov 9 layer. Could not see all the results due to limited visibility. A backcountry natural avalanche cycle from a 2-3days ago from rain and warm temperatures is expected.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few explosive triggered avalanches up to size 2 were observed at Sunshine Village today failing on the basal crust/facet combination. No new natural avalanches were observed today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported in the forecast region today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported in the bulletin region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has decreased with the arrival of cold temperatures. No new avalanches were observed yesterday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported in the forecast region today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported in the forecast region today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has slowed down but there is plenty of evidence of large deep slides in wind loaded features that have released in the last cycle. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only minor loose dry activity with the new snow running over the surface crust has been seen.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported in the forecast region today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There were many ski tracks going into more aggressive alpine terrain in the Bow Summit area today. A large size 2.5 natural avalanche was also noticed on a NW aspect of Observation subpeak. This looked to be recent within the last 48 hours and is indicative of the low probability/ high consequence conditions we are currently dealing with.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has slowed down but there is plenty of evidence of large deep slides in wind loaded features that have released in the last cycle. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There were many ski tracks going into more aggressive alpine terrain in the Bow Summit area recently. A large size 2.5 natural avalanche was also noticed on a NW aspect of Observation subpeak. This looked to be recent within the last 3 days and is indicative of the low probability/ high consequence conditions we are currently dealing with.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today, but there is evidence of large deep slides in wind loaded features that have released in the last cycle. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed since Dec 12th. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported in the Little Yoho region recently.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was noted today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations today. There is past evidence of large deep slides in wind loaded features that released in the last cycle. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches occurred yesterday. On the 16th skiers accidentally triggered a small avalanche on the fan of the Forever Young Couloir, in a shallow rocky area. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been seen or reported</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity although snowpack tests at treeline today did not inspire confidence in the mind set of today's avalanche forecaster.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No observations in the Marmot area today.  No other avalanches reported. There is past evidence of large deep slides in wind loaded features that released in the last cycle. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was noted today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the Highway Corridor. We received a report of a natural avalanche in Cheops North #4, running to the creek in Connaught Creek drainage. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cracking of new snow in immediate lees and soft slabs to size 1 reported in the Lake Louise area today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some minor loose snow sluffing on steep terrain.  No slab avalanches reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A backcountry report of a skier triggered size 1.5 avalanche,10-15m wide, 10-15cm deep, from Balu Pass, northeast aspect, at ~2000m on a convex roll just below the ridge. 6 size 2.0 natural slab avalanches observed yesterday east of the Rogers Pass summit in the highway corridor. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cracking of new snow in immediate lees and soft slabs to size 1 reported in the Lake Louise area today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cracking of new snow in immediate lees and soft slabs to size 1 reported in the Lake Louise area today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field team on Mt Fidelity, 1900m to 2100m, reporting touchy conditions with several skier remote and control triggered size 1.0 and 2 size 2.0 avalanches with wide propagation down 30cm running on the Dec 17 surface hoar/crust layer. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> Numerous size 2.0 natural slab avalanches observed yesterday east of the Rogers Pass summit in the highway corridor</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a few storms slabs to size 2 could be seen at treeline. Small settlements were also felt by forecasters on patrol near treeline.&nbsp; In alpine areas a few recent slabs could be seen in the lee areas, the North and East aspects, of steep alpine features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanche activity was noted.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous skier triggered and natural avalanches were observed or reported yesterday. Remote triggering of the surface slab from distances greater than 50m were reported. Most of the activity was occurring between 1700-2400m. One reported skier triggered slide propagated over 200m. This avalanche activity should be expected to continue today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche observed or reported today, however, we expect to see a small cycle within the next 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In Yoho backcountry several avalanches up to Class 2.5 (with propagations up to 200 m) were observed running in recent storm snow. Lake Louise ski hill reported several natural and skier controlled avalanches running in the storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Three new avalanches were recorded in the Columbia  Icefields area. The events were  size 2 thin storm slabs and class 1.5 point releases from steep slab alpine terrain.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier triggered, skier remote and natural avalanches continued through Dec 23. Remote triggering of the surface slab from distances greater than 50m were reported Dec 22. Most of the activity was occurring between 1700-2400m. Moderate to strong southerly winds will be continuing to transport storm snow and overload the Dec 17 surface hoar layer. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was seen on Wednesday but visibility was poor with the incoming storm. There has likely been some activity on steep terrain in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">In Yoho backcountry several avalanches up to Class 2.5 (with propagations up to 200 m) were observed running in recent storm snow. Lake Louise ski hill reported several natural and skier controlled avalanches running in the storm snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several avalanches up to Class 2.5 (with propagations up to 200 m) were observed running in the recent storm snow in Yoho Park on Dec 24th. Lake Louise ski hill also reported several natural and skier controlled avalanches up to size 2.5 within the past 48hrs, running in the new storm snow and occasionally stepping down to the basal facets/crusts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today. We did, however, receive numerous calls this morning from local residents reporting sleigh and reindeer tracks on snow covered roof tops.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday triggered 16 size 3 to 3.5 avalanches, including this one off the </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://data.avalanche.ca/Images/Moccasin%20Flats%202014-12-24.pdf" target="_blank"><span class="s_9255B882">West face of Cougar Mountain</span></a><span class="s_AA239A9B">, and over 20 size 2's. Wide propagations were observed. Recently skier triggered and skier remote triggering of the slab from over 50m away continue to occur. Most of the activity was occurring between 1700-2400m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several avalanches up to Class 2.5 (with propagations up to 200 m) were observed running in the recent storm snow in Yoho Park on Dec 24th. Lake Louise ski hill also reported several natural and skier controlled avalanches up to size 2.5 within the past 48hrs, running in the new storm snow and occasionally stepping down to the basal facets/crusts.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">&quot;</span><a href="https://www.facebook.com/ParksMountainSafety/photos/a.745152068868118.1073741868.145133538869977/765954363454555/?type=1&amp;theater" target="_blank"><span class="s_9255B882">Speed Run</span></a><span class="s_AA239A9B">&quot; at Lake Louise ran naturally as a size 2 on December 26th following some moderate wind transport overnight. A couple other natural avalanches up to size 2 were also observed. Following the storm last week avalanches up to size 2.5 were observed with propagations up to 200 m, and occasionally stepping down to the basal facets/crusts. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very thin loose snow avalanches observed on East and West alpine aspects from steep rocky terrain. Some very thin slab avalanches (Size 0.5) on reversed cross-loaded gulley features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday1 natural avalanche size 2.5 east of the Rogers Pass summit north aspect from one of the gullies off of Mt Macdonald. Artillery control from two days ago produced numerous avalanches up to size 3.5 showing wide propagation within the highway corridor. Some stepping down to deeper layers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">&quot;</span><a href="https://www.facebook.com/ParksMountainSafety/photos/a.745152068868118.1073741868.145133538869977/765954363454555/?type=1&amp;theater" target="_blank"><span class="s_9255B882">Speed Run</span></a><span class="s_AA239A9B">&quot; at Lake Louise ran naturally as a size 2 on December 26th following some moderate wind transport overnight. A couple other natural avalanches up to size 2 were also observed. Following the storm last week avalanches up to size 2.5 were observed with propagations up to 200 m, and occasionally stepping down to the basal facets/crusts. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Following the storm last week avalanches up to size 2.5 were observed with propagations up to 200 m, occasionally stepping down to the basal facets/crusts.There was significantly less avalanche activity around the Banff area. The Lake Louise region and West received the bulk of the snow with a subsequent increase in activity.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported in forecast area</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Backcountry report from top of Grizzly Shoulder to Puff Daddy, NE facing bowl feature, remotely triggered size 2.0 avalanche, ~2000m, down 50cm, 40-50m wide, 100m long. A second report of a rider triggered avalanche size 1.5 down 55cm and 10-20m wide from another feature in the same area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier triggered size 1.5-2 avalanche was reported today in the Wizard Chutes near Healy Creek at approximately 1900m. It started as a small wind slab near tree line and then stepped down to the basal facets. Other small skier and explosive triggered wind slabs have been reported by the local ski areas in the last 48hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Backcountry report from yesterday at Balu Pass, east aspect, 200m wide avalanche, trigger unknown, ran to bottom flats. Teddy Bear trees, remote size 2.0, east aspect, 70-100cm deep. Slope to Puff Daddy, NE aspect, rider triggered size 1.0, ~1930m,  below a remotely triggered size 2.0 avalanche from two days ago, ~2000m, 75m wide, 75m long. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The new snow is hiding any evidence of  recent avalanche activity however at least one large natural was seen between the storms on Friday.  This slab failed just beneath the cornice above Forum lake, 100m wide and pulled several other slabs as it scoured down the steep alpine face.  Reports of skier triggering continue in nearby areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier triggered size 1.5-2 avalanche was reported last Sunday in the Wizard Chutes near Healy Creek at approximately 1900m. It started as a small wind slab near tree line and then stepped down to the basal facets. Other small skier and explosive triggered wind slabs have been reported by the local ski areas prior to the cold snap.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported in the forecast area. There was good visibility into the alpine from Jasper to Saskatchewan crossing.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, several ski cuts, size 1 and whumphs observed by the field team on Mt Abbott between 1800-2000m. Backcountry report from Hospital Knob area in Connaught of several skier triggered and remote avalanches to size 1.5. Daily reports of rider triggered avalanches to size 2.0 over the last week all down ~50cm on the Dec 17 surface hoar.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">&quot;</span><a href="https://www.facebook.com/ParksMountainSafety/photos/a.745152068868118.1073741868.145133538869977/765954363454555/?type=1&amp;theater" target="_blank"><span class="s_9255B882">Speed Run</span></a><span class="s_AA239A9B">&quot; at Lake Louise ran naturally as a size 2 on December 26th following some moderate wind transport overnight. On the 27th, skiers triggered a small slab in Wizard Chutes (Sunshine region) and it stepped down to the basal facets yeilding a size 2.5 avalanche.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday skiers triggered a size 2 skinning up Youngs Peak. The 1m deep windslab propagated 150m wide and ran 300m. No-one was involved. Over the past week there have been daily reports of rider triggered avalanches to size 2.0 failing on the Dec 17 surface hoar. Many of these have been remotely triggered, and sometimes triggering slopes overhead. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There continue to be daily reports of rider triggered avalanches failing on the Dec17 surface hoar. Many have been remotely triggered, sometimes triggering slopes overhead. Yesterday, skiers triggered small slabs descending from Lookout Col, and Monday skiers triggered a size 2 ascending Youngs Peak. The </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://data.avalanche.ca/Images/Youngs%20Peakx%20crown.pdf" target="_blank"><span class="s_9255B882">1m deep windslab was 150m wide</span></a><span class="s_AA239A9B"> and </span><a id='GoToAdded' href="http://www.pc.gc.ca/apps/links/goto_e.asp?destination=http://data.avalanche.ca/Images/Youngs%20Peak%20debris.pdf" target="_blank"><span class="s_9255B882">ran 300m</span></a><span class="s_AA239A9B">. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported. A large settlement was observed on the Dec 18 surface hoar down 30 cm by a group en route to Isolated Col. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skier and rider triggered avalanches were reported in the last 48hrs on the December 17th layer below Lookout Notch.  A recent size two slab avalanche was observed from a distance on the Balu headwall the trigger is unknown.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The new snow is hiding any evidence of recent avalanche activity however at least three large avalanches occurred during the last storm. Natural avalanche activity seems to have tapper off for no but could increase with new snow forecast for Sunday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported. A large settlement was observed on the Dec 18 surface hoar down 30 cm by a group en route to Isolated Col. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today. On Dec 31, a thin size 1 windslab was triggered by a group on </span><a href="https://www.facebook.com/ParksMountainSafety?ref=aymt_homepage_panel" target="_blank"><span class="s_9255B882">Quartz ridge</span></a><span class="s_AA239A9B"> near Sunshine Ski Area.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has decreased in recent days but this is likely to change. New overnight snow and wind will form touchy storm slabs on exposed features. There is now increased risk of avalanches stepping down 60-70cm to the December 17 surface hoar layer, which is still reactive to skier loads. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported. A large settlement was observed on the Dec 18 surface hoar down 30 cm by a group en route to Isolated Col (on Thursday) and by groups in the Emerald slide path (on Friday).  Anything starting to slab up with wind effect seemed to produce the settlements.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed in the forecast area. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The December 17 surface hoar layer produced a large skier triggered avalanche yesterday on a north aspect at treeline on surface hoar buried 60cm. New snow from the past 48 hours remains powdery in most locations producing small loose avalanches. This storm slab is expected to gain cohesion with forecasted winds and precipitation. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.. Over the last few days, many features starting to slab up with wind effect have been producing &quot;whumpfs&quot; over the dec 18th layer at treeline and above</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The debris of a size one slab avalanche observed in the Winston Churchill Range which ran on a steep west facing aspect in the last 24 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, in the highway corridor 3 natural avalanches, size 2 to 2.5. 2 days ago, there was a size 2 skier triggered avalanche on a north aspect at treeline on surface hoar buried 60cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported.. Over the last few days, many features starting to slab up with wind effect have been producing &quot;whumpfs&quot; over the dec 18th layer at treeline and above</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, a size 2.0 skier accidental avalanche in Teddy Bear trees. East aspect, ~2000m, ~35 degrees, ~65cm deep, 40-50m wide, ~150m long. Avalanche was triggered near the ridge crest and rider went for a ride through the trees. Slabs pulled out lower down as well. Several large natural avalanches within the highway corridor early this morning.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Monday I triggered a south facing 40 degree slope at treeline by taking off my skis to dig a profile at the top of the start zone. Thankfully, only a 10cm crack formed at the crown in front of my feet, however cracks could be seen up to 50m away down the slope. Subsequent tests produced easy sudden planar shears on facets above the Dec 13 Crust. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been observed or reported yet, but extensive avalanche activity has been reported to the west, which is a good indication of what to expect in the Little Yoho region.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several avalanches observed in the Field area, including one that ran over the ice climb Pilsner Pillar and another one from the Mt. Stephen cliffs that put 2.5 meters of debris on the railroad. Very limited observations from field teams and the ski areas today due to poor visibility.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous size 2 to 2.5 avalanches with the occasional size 3 avalanche along the highway corridor. Skiers, sluff management will be important on steeper features at and below treeline. At and above treeline expect new storm slabs and always keep in mind the Dec 17th weak layer which will be getting overloaded by this large storm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed or reported in this region today, but visibility was terrible.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control in Kootenay and Yoho Park produced between 10-15 avalanches between size 2 and 3. Mostly size 2's with a couple of larger ones. Human triggering is very likely at this time.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Last nights warm conditions has turned the recent storm snow into a touchy slab. Field teams were able to trigger several small soft slabs to size 1. Two other small slides were reported off steep rocky terrain at lower elevations (BTL).</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control yesterday produced numerous size 2 to 3.5 slides with most slides coming in at size 2.5. The larger slides were digging down to the Dec 17th layer.  A natural avalanche cycle had occurred early in the morning of January 6th with slides up to 2.5 in size initiating in the storm snow at alpine elevations.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control in Kootenay and Yoho Park produced between 10-15 avalanches between size 2 and 3. Mostly size 2's with a couple of larger ones. Human triggering is very likely at this time.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterdays avalanche control produced numerous large avalanches and some continued natural activity today would indicate that things have not yet settled. Today's activity included avalanches to size 2 starting in steep terrain and stopping in the track.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The debris of a natural size 2 storm slab avalanche was observed from East facing terrain in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The sun came out yesterday and for a short time around 11am the solar radiation was intense resulting in a few solar triggered avalanches on steep solar aspects. These slides were confined to the recent storm snow.  The sun is expected to come out again today so steep solar aspects should be avoided. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temperatures and strong winds induced a widespread cycle of storm slabs on all aspects and elevations Wednesday. Some of these events ran from ridge crest to valley bottom however with our first look around today we saw no evidence of activity on the persistent weak layer. There have however, been reports of activity on the PWL from neighbors. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control a few days ago produced a few large avalanches and some continued natural activity yesterday. Today's activity near Lake Louise included avalanches in the size 2 to size 3 range.  These avalanches are being initiated at the Dec 18th interface and in steep, large scale terrain features are stepping down to ground.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche cycle is being reported from field teams with multiple slides, up to sz 3 on south to westerly (solar) aspects over the last 2 days. A dramatic temperature inversion at around 2500ms (cold air low/warm above) is affecting the slopes and seems to have enough punch to initiate the natural activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has begun to taper off since the storm, however isolated size 2 avalanches continue to be observed on steep terrain in the highway corridor. Yesterday a field team on Mt Abbott was able initiate a Sc size1.5 on a convex roll near treeline. The failure plane was the Dec 17 surface hoar, which had previously released and reloaded.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural activity was noted today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off but human triggering remains likely. A size 1.5 skier triggered avalanche occurred in the Wizard Chutes near tree line Jan 10th in the Sunshine area. Avalanche control at Lake Louise on Jan 9th resulted in a size 3 which initiated on the Dec 18th interface and then stepped down to facets near the ground. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle up to sz 3 on south to westerly (solar) aspects occurred over the week. A dramatic temperature inversion at around 2500ms (cold air low/warm above) was actively affecting the slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural activity has tapered off since the storm the last storm cycle. A skier controlled avalanche size 1.5 occurred on Thursday on the December 17th surface hoar layer, buried down 60-80cm. This layer has been most reactive around treeline.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off but human triggering remains likely. A size 1.5 skier triggered avalanche occurred in the Wizard Chutes near tree line Jan 10th in the Sunshine area. Avalanche control at Lake Louise on Jan 9th resulted in a size 3 which initiated on the Dec 18th interface and then stepped down to facets near the ground. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed or reported today. However, conditions are still touchy.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported or observed. Some collapses within the snow pack felt while touring up through the trees with no observable cracking. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 2.0 skier triggered avalanche in Loop Brook area, east aspect moraine feature, at 1700m, down ~60cm on the Dec 17 surface hoar layer, 4-6mm in size. 50m wide and 100m long. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flights over the park today with good visibility revealed a widespread natural avalanche cycle over the past 48-hours. Wide propagations at treeline and above up to size 3, many running to the bottom of the runout zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Warm day time temps will likely increase avalanche risk on solar aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">From two days ago, size 2.0 skier triggered avalanche in Loop Brook area, east aspect moraine feature, at 1700m, down ~60cm on the Dec 17 surface hoar layer, 4-6mm in size. 50m wide and 100m long. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Despite seeing very little activity over the last few days we observed a significant slab about  40m wide, 80 to 100 cm deep on steep north facing cliffy terrain near ridge top. This slab likely failed on the Dec 13 persistent weak layer although it may have been triggered by a smaller slab and illustrates the need for care with this layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flights over the park today with good visibility revealed a widespread natural avalanche cycle over the past 48-hours. Wide propagations at treeline and above up to size 3, many running to the bottom of the runout zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flights over the park today with good visibility revealed a widespread natural avalanche cycle over the past few days. Wide propagations at treeline and above up to size 3, many running to the bottom of the runout zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Overcast skies will prevent the solar effect that was originally expected for the area in the alpine.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two size 2 natural avalanches were observed yesterday from steep north facing terrain. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">On the weekend there was a size 2.0 skier triggered avalanche in Loop Brook area. It was on an east aspect moraine feature, at 1700m, failing down ~60cm on the Dec 17 surface hoar layer 4-6mm in size, and was 50m wide and 100m long. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flights over the park today with good visibility revealed a widespread natural avalanche cycle over the past 36-hours. Wide propagations at treeline and above up to size 3, many running to the bottom of the runout zones.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity observed on a field trip to the Helen Shoulder area</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the forecast zone. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sporadic avalanche activity continues. Small, loose solar triggered avalanches have been observed daily and there were two size 2's from North aspects yesterday. Outside the park a skier was caught in a size 2 when the Dec 17 failed on an unsupported roll. On the weekend a size 2 was ski cut on a moraine which failed on the Dec 17 surface hoar.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanche activity observed in past 48 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temps have triggered a few small storm / wind slab avalanches at TL and BTL within the past 24h in the south of the forecast region. No new avalanches were observed in the north of the forecast region. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been a few solar triggered surface slides observed each day this week at alpine and treeline elevations. Two size 2 slabs occurred on North aspects Tuesday and last weekend a size 2 was ski cut on a moraine feature up Loop Brook.  These slabs all came out on the December 17th layer. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported on Jan 15.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported in last 48 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanche activity observed in past 72 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed in the forecast region today. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported in last 48 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanche activity observed in past 72 hrs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One large avalanche observed running on steep rock slabs on Whistler Mountain which was likely triggered by redistributed blowing snow. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several large natural avalanches were observed yesterday during in paths facing the highway corridor. This avalanche cycle was a result of a developing storm slab in recent new snow. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported in last 72 hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Although visibility was too poor to see any natural activity, skiers were able to easily trigger freshly formed windslabs today in any open lee features at Treeline and above.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 avalanche observed in the south of the forecast region. No other avalanches observed in the rest of the forecast area.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skiers were able to easily trigger the sensitive new windslabs that have formed at Treeline and above today in neighboring areas. These  soft slabs propagated up to 20m and were up to 40cm deep. Poor visibility made it difficult to see further evidence of avalanche activity. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On an avalanche control flight today to the Sunshine road, 8 of 9 shots produced significant avalanches and 3 natural avalanches were observed. Most of these initiated in the recent storm slabs 20 cm deep but several also stepped down to the Dec 18 interface to a depth of 50cm. Crowns were as wide as 150m and several events ran up to 1km.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The debris of several size 2.5 avalanches were observed in the south of the forecast region today, starting from cross loaded features in the alpine. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Backcountry users and field teams reporting several remote and rider triggered avalanches to size 1.5 down 20-50cm running on the Jan 15 surface hoar layer. Cheops North 4,natural avalanche dusted two riders on the uptrack. Natural avalanche cycle up to size 3.0 within the highway corridor began yesterday afternoon and into early this morning.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported on Jan 15.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On an avalanche control flight today to the Sunshine road, 8 of 9 shots produced significant avalanches and 3 natural avalanches were observed. Most of these initiated in the recent storm slabs 20 cm deep but several also stepped down to the Dec 18 interface to a depth of 50cm. Two size 1.5 naturals were observed on Labbat's Lane and Pilsner Pillar</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but human and explosive triggered avalanches persist.  Yesterday someone in the Sunshine Village backcountry triggered a windslab that took them for a 50m ride. Avalanche control on Mt Dennis in Field today produced no slabs, but loose snow avalanches ran 1000m over Pilsner Pillar.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle occurred yesterday and into last night. Large avalanches up to size 3 were observed and reported yesterday afternoon both in the back country (Connaught Creek) and the highway corridor. Human triggered slides were reported on McGill two days ago. The January 15 layer is touchy and reactive. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed or reported on Jan 15.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but human and explosive triggered avalanches persist. Yesterday someone in the Sunshine Village backcountry triggered a windslab that took them for a 50m ride. Avalanche control on Mt Dennis in Field today produced no slabs, but loose snow avalanches ran 1000m over Pilsner Pillar.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but forecasters on Mt. Field reported a couple large whumphs in an open area below treeline, indicating human triggering of deeper weak layers is still possible in the right terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches observed in maligne and hwy 93</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Artillery control yesterday triggered over 30 size 2 to 3.5 avalanches from all aspects between 17-2700m. Notables were size 3.5's from the W face of Cheops and off Mt Tupper that ran into the creeks. Avalanches up to size 3 have been observed in the backcountry. Human triggered avalanches continue in the region with remote triggering up to 300m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but forecasters on Mt. Field today experienced a large whumph in an open area at 1850m indicating the deeper layers are still reactive to human triggering in some areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but forecasters on Mt. Field reported a couple large whumphs in an open area below treeline, indicating human triggering of deeper weak layers is still possible in the right terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The sun came out in the afternoon and triggered a size 2 slab avalanche in a shallow alpine gully feature on a west facing aspect indicating that the sun is gaining strength. Below treeline, road cutbanks facing the south are creating snowballing and small loose avalanches.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday artillery control triggered over 30 size 2 to 3.5 avalanches from all aspects between 17-2700m. Notables were size 3.5's from the W face of Cheops and off Mt Tupper that ran into the creeks. Human triggered avalanches up to size 2.5 continue to occur in the region. Remote triggering from up to 300m has been reported.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was evidence of wind slab avalanches at the back of Forum lake but this was likely from a few days ago. Otherwise there has been no avalanche activity observed up to Jan 22.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed, but forecasters on Mt. Field today experienced a large whumph on Wednesday in an open area at 1850m indicating the deeper layers are still reactive to human triggering in some areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed in the last 48 hrs. We are still experiencing whumphs in some open areas below tree line in the Little Yoho region indicating human triggering of deeper weak layers is still possible in the right terrain. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No new avalanches reported, yet!</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday artillery control triggered over 30 size 2 to 3.5 avalanches from all aspects between 17-2700m. Notables were size 3.5's from the W face of Cheops and off Mt Tupper that ran into the creeks. Human triggered avalanches up to size 2.5 continue to occur in the region. Remote triggering from up to 300m has been reported. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No natural avalanches observed in the last 48hrs. Forecasters on Mt. Field on Jan 21st experienced large whumpfs in an open area at 1850m indicating the deeper layers may still be reactive to human triggering in some areas.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches were reported today. Notably, the bowl above the Urs hole ice climb on Cascade Mountain had numerous natural avalanches, with one size 3 stepping down to the basal weakness. This was likely triggered by sun. Wind loading in other alpine areas which received more snow saw isolated avalanches to size 2 on lee aspects.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 slab avalanche occurred today in the Parker ridge area by a skier.  This happened on a NE aspect at treeline. Below treeline, there were numerous size 0.5 to 1 loose snow avalanches going to ground as a result of the overnight rainfall. Many of these locations had less than 20cm of snow on the slope. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are currently experiencing a widespread natural avalanche cycle from 40cm of new snow in the past 24 hours and strong southerly winds. Numerous natural avalanches up to size 3 were observed in the highway corridor during the overnight period. Avalanches are likely propagating on the January 15 surface hoar down layer down 80-100cm. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Sloughing and loose, wet avalanches up to size 1.5 were observed out of steep, rocky terrain.  Limited observations in the area today.  </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches were observed and reported today with slabs up to size 2.5 at tree line and above and loose wet slides up to size 2 below tree line in all of the forecast region. Notably Cascade Falls, Rogans Gully, Bourgeau L &amp; R and many of the climbs in Field all saw avalanche activity today. We expect this cycle to continue tomorrow </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avi control in the Icefields produced numerous size 1's up to a size 2.5 slabs with impressive propagation over 200ms on a NE aspect at TL. Wet avalanches BTL are entraining the storm snow, building mass and moving fast from the rocks. Ice climbs are wet and becoming detached from the rock. Of note, the Pencil on Polar Circus broke off today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, natural avalanches and artillery control produced numerous size 2.0 to 3.0 avalanches within the highway corridor. Backcountry observations are limited at this time but expect a natural cycle to have occurred. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A significant solar cycle occurred Saturday with loose wet sluffs initiating at treeline elevations and triggering recent windslabs, persistent slab,  and basal facets in thin snowpack areas to size 2. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches were observed and reported today with slabs up to size 2.5 at tree line and above and loose wet slides up to size 2 below tree line in all of the forecast region. Notably Cascade Falls, Rogans Gully, Bourgeau L &amp; R and many of the climbs in Field all saw avalanche activity today. We expect this cycle to continue tomorrow </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread avalanche cycle occurred on Sunday with dozens of large avalanches observed on all aspects, and at all elevations with lower elevations being particularly active. Monday saw less activity, but avalanche control near Mt Wilson produced a large avalanche onto the 93N highway. Avalanches continue to be reported every few hours.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Numerous slab avalanches up to size 3 were seen originating at treeline on all aspects near the forecast area. These were often started by a point release from above which would have stepped down to the midpack weak layer and also to ground.&nbsp; Below treeline, numerous loose snow avalanches up to size 2,started from rock bluffs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday a natural cycle with warm temperatures and rain; numerous avalanches up to Size 3 in highway corridor, some gouging to ground at low elevation and loose avalanches triggering slabs. A back country report from a low elevation Size 2 natural avalanche 15m wide, 200m long, 50-60cm deep, in the Asulkan area close to the Abbott slide path.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The peak of the current avalanche cycle occurred on Sunday, when dozens of large natural avalanches were observed, including the path beside the Emerald Lake Slide Path.  The gullies in Field all produced wet avalanches running over the ice climbs.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The warm temperatures created a widespread avalanche cycle on Sunday and Monday. Tuesday saw slightly cooler temperatures and less natural activity. Avalanches observed were restricted to isothermal avalanches in shallow snowpack areas below treeline.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Avalanche control, at and above treeline, produced numerous slab avalanches up to size 3 along the icefield parkway. At times the avalanche was triggered before the explosives detonated. Below 1,800m moist point release to size 2 are traveling to mid runout. and taking the snowpack to ground.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity tapered off yesterday when the rain stopped but a few loose wet avalanches to size 2 were observed in the Hermit drainage. Avalanche control triggered slab avalanches to size 3 failing on the Jan 15th layer. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The warm temperatures created a widespread avalanche cycle on Sunday and Monday. Tuesday saw slightly cooler temperatures and less natural activity. Avalanches observed were restricted to isothermal avalanches in shallow snowpack areas below treeline.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow study flight East of the divide saw lots of previous activity up to size 3, with no new avalanches. The field trip to Lake Ohara saw only small wet slabs at treeline and below from last weekends cycle. The big alpine peaks had no visible activity with good visibility. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> The avalanche activity has slowed with the cooler temperatures.  Several slab avalanches to size 2.5 from the past 24 hrs  were observed on easterly aspects around 2400 m.  Previous loose wet avalanches were numerous on lower elevation westerly aspects and pin wheeling was observed up to 2300 m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity has tapered off with cooling. Recent avalanche control triggered slab avalanches to size 3 failing on the Jan 15th layer. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported in the Little Yoho region today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> The avalanche activity has slowed with the cooler temperatures. Several small loose wet slides were observed today along the Endless Chain out of steep, rocky, solar aspects around 2100m.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches were observed yesterday. An artillery verification shoot with 2 rounds produced a size 1.5 and a size 2 avalanche in previously controlled paths. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Now that temperatures have cooled down natural avalanche activity has diminished however skier triggering remains a concern in specific areas : Treeline and above on shaded slopes.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported today. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been very little natural activity in the past few days with the exception of some size 2 explosive results yesterday in Lake Louise. Human triggered avalanches are still possible and cautious terrain selection is still strongly advised in spite of the Low rating.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Poor visibility today. Touchy cornices have been observed and reported in the past 48 hours. Some cornice falls triggered slabs up to size 2 at the ski hill during recent natural cornice failures.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A small solar avalanche cycle yesterday afternoon released a size 2 on Avalanche Crest. Several small solar releases were observed on step S-SW aspects around exposed rocks and cliff areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was observed or reported today, however one explosive result up to size 2 out of a steep &amp; complex alpine feature was reported by Lake Louise yesterday so avalanches are still possible out of steep, rocky alpine terrain in isolated terrain features with larger triggers.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some minor sloughing of the new snow out of cliffed terrain, triggered by sun. No new avalanches observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">An avalanche cycle has taken place in the last 24 hrs. Numerous solar triggered size 2 slab and loose snow avalanches at tree line and sub alpine on W aspects failing on the rain crust.  3 size 2 slab avalanches on E aspects  failing on rain crust at tree line and above. Size 3 explosive triggered avalanche at Marmot stepped down to Nov crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were observed yesterday, but small cycles have been occurring on steep S-SW aspects around exposed rocks and cliff areas during warm sunny periods in the past few days. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today by field teams in the Columbia Icefield area and from the lands adjacent to Marmot Basin. Visibility was very poor due to cloudy conditions and snowfall.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, there was a report of a human triggered avalanche, size 1.5 at Bruins Pass into 8812 Bowl off the east ridge of 8812 Peak ~2700m, SE aspect, 15-20cm deep. Along the highway corridor there were was one loose natural avalanche size 1.5 east of the Rogers Pass summit.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was observed or reported today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose snow sluffing from cliff areas was observed today, but no new slab avalanches were reported or observed.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported today. Visibility was poor due to cloudy conditions and snowfall.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed yesterday.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Technicians traveling near the divide today found new windslabs above the hard crust to be sensitive to ski cutting. Otherwise, no activity has been seen in the last few days since the snow refroze after last week's warm up.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose snow sluffing out of cliffs was observed in numerous locations today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A large natural occurred on Mt. Stephen sometime in the last 24 hours. This was likely due to localized wind loading in the area overnight. There is a lot of low density snow available for transport so conditions can change quickly if wind is present.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field team in the Icefields area today reported three size 2 and one size 2.5 slab avalanches in cross loaded features in the alpine. The size 2.5 stepped down to the November basal facet layer.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous avalanches occurred in the highway corridor in the size 1 to 2 range.  These slides were mainly found in steep gully features.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Technicians traveling near the divide today found new windslabs above the hard crust to be sensitive to ski cutting. Otherwise, no activity has been seen in the last few days since the snow refroze after last week's warm up.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Multiple large loose dry avalanches out of steep terrain occurred overnight in the Emerald Lake area. These started as sluffs and gathered mass, running quite far. A large natural occurred on Mt. Stephen sometime in the last 24 hours. All of these were likely caused by localized wind loading in the area overnight. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural size 2 avalanche was observed on Mt. Redoubt near Lake Louise, approximately 60 m wide and failing on the ground level depth hoar.  Good backcountry observations were made from Sunshine Village and the Brewster Creek area, and no new avalanches were observed here.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed along the Icefields Parkway today.  Good visibility. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday, skiers accidentally triggered a size 2.5 avalanche from a SE aspect at 2120m. The avalanche propagated ~200m wide and ran up to 600m. Along the highway one size 3 and numerous size 2-2.5 natural avalanches were observed, occurring from all aspects generally above 1800m. Recent activity is occurring on the Jan 30 crust.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported or observed in this region today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
.s_9255B882 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #0000FF;text-decoration: underline; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural size 2 avalanche was observed on Mt. Redoubt near Lake Louise yesterday which stepped to the basal weakness, was 60 m wide and failed on the ground level depth hoar. Another group today triggered a size 2.5 which was almost 2m deep on a crossloaded treeline feature above Bow Summit.  </span><a href="https://www.facebook.com/ParksMountainSafety/photos/a.745152068868118.1073741868.145133538869977/786812438035414/?type=1&amp;theater" target="_blank"><span class="s_9255B882">Yikes</span></a><span class="s_AA239A9B">!  This failed on the Basal facets/Depth hoar.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Road patrols reporting poor visibility and no new avalanches observed. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light winds and flurries didn't add enough load to trigger many avalanches yesterday. There were a few natural avalanches to size 2 observed. Small slabs triggered by skiers indicated that the slab is forming. On Tuesday skiers accidentally triggered a size 2.5 avalanche from a SE aspect at 2120m. The avalanche propagated ~200m wide and ran ~600m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small slabs of snow failing between skier's tracks were the only indication seen while skiing today that there may be trouble ahead with the bond of the new snow to the crust. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunshine village was reporting skier controlled storm slabs to size 1 in open alpine regions. These were running on the Jan 30 interface. No avalanches were observed in the Mt. Field area, only sloughing in steep (40+ degree) ski terrain.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural size 2.5 avalanche narrowly missed a number of snow-shoers today in Lake O'Hara out the Schaeffer Bowl area. Several large avalanches up to size 3 were observed on the Highway 93S. Poor weather and embedded fog limited the forecaster's observations today but there were undoubtedly many more avalanches occurring than were seen today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Currently experiencing an avalanche cycle at all elevations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Natural avalanche cycle and avalanche control in progress along the highway corridor producing avalanches to size 3.5. Avalanches begin dry and end as moist onto their fans. On Tuesday skiers accidentally triggered a size 2.5 avalanche from a SE aspect at 2120m. The avalanche propagated ~200m wide and ran ~600m. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">One natural size 2.5 avalanche nearly struck snow-shoers today in Lake O'Hara in the Schaeffer Bowl area. Several large avalanches up to size 3 were observed in Kootenay Park. Ski areas in the Rockies were reporting numerous natural and explosive controlled Storm Slabs up to size 2.5 today some failing on the November 6th facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control on Mt. Whymper today produced avalanches up to size 2.5. Fracture line thickness varied between 20 and 60cm with average running distance about 250m. Also, evidence of a widespread cycle up to size 3 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle with slides up to 3.5.  Avalanche control efforts along the Icefields Parkway produced large avalanches one bring down mature timber and burying the road.  Several avalanches initiated with just the weight of the bomb on the slope. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday saw a widespread natural cycle producing large avalanches with moist deposits at lower elevations. Artillery highway avalanche control produced numerous size 3-3.5 avalanches with with wide propagating slabs on all aspects. Avalanches ran far, in some cases to the end of the run outs. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were reported or observed directly in the Little Yoho region, however, Mt. Dennis (adjacent to Little Yoho) had an extensive cycle early this morning, up to size 3. It is suspected that a major avalanche cycle has effected Little Yoho region today.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control today in Yoho Park and Koorenay Park produced numerous avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also, evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The natural avalanche cycle continues with slides up to 2.5 involving the new storm snow. Avalanche control efforts along the Icefields Parkway produced large avalanches around Polar Circus. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observed several new large natural avalanches yesterday in the Highway Corridor. Most of the new slides began dry and ended moist, terminating farther than previous artillery triggered avalanches and in some cases gouging into existing debris.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control today in Yoho Park and Koorenay Park produced numerous avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also, evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control over the past three days in Banff, Yoho Park and Koorenay Park have produced numerous avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also, evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Minor sluffing of loose dry snow out of steep terrain.  No new observations.  </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Backcountry users reported hearing avalanches in Connaught yesterday but could not confirm the exact size and location. There is large avalanche debris to the valley bottom in Grizzly slide path in Connaught from the last 48 to 72hrs. Yesterday there were 3 moist natural avalanches, size 2.0 in the highway corridor. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was a great deal of avalanche activity over the weekend. With the rapid loading and winds, storms slabs to sz 2.5 failed above the Jan 31 crusts treeline and above some as a result of cornice failures. Below treeline surface crusts broke down with the rain allowing loose wet activity and a few wet slabs failing on the Dec 13 crust layer, </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control over the past three days have produced numerous slab avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also there was evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control over the past four days in Banff, Yoho Park and Kootenay Park have produced numerous avalanches up to size 3. Most of the avalanches started dry and turned wet at lower elevations. Also, evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Minor sluffing continues out of steep terrain. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Rain switched to snow yesterday and avalanche activity tapered off. Since Thursday, a large avalanche cycle occurred with avalanches to size 3.5 running from all elevations into valley bottoms. Reports from skiers in the region are of touchy conditions, with remote triggering of slabs up to 1m deep and wide propagations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control over the past three days have produced numerous slab avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also there was evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control over the past four days in Banff, Yoho Park and Kootenay Park have produced numerous avalanches up to size 3 over the last 4 days. Most of the avalanches started dry and turned wet at lower elevations. Also, evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Minor sluffing continues out of steep terrain. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity continues during periods of precipitation, with large avalanches running into fans.  Reports from skiers in the region are of touchy conditions, with remote triggering of slabs up to 1m deep and wide propagations. Below 1500m moist snow is touchy and easily triggered by skiers, especially on steep gully like features. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent avalanche control produced numerous slab avalanches up to size 3. Many of the avalanches started dry and turned wet at lower elevations. Also there was evidence of a widespread cycle up to size 3.5 throughout the forecast region. Some avalanches were running close to full path.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity is tapering as the snowpack slowly adjusts to the new load. However, moderate to hard sudden collapse snowpack tests today in the Bow Summit area indicate skier triggering is still very possible. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two size 2 slab avalanches were observed around treeline today on low angle northerly aspects. It is likely that these avalanches failed on a surface hoar layer sitting on the January 30 rain crust.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2 loose wet avalanche was observed yesterday in the highway corridor on Tupper Minor avalanche path east of Rogers Pass.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cornice fall triggered thin windslabs that were enough of a load to pull a 100m wide slab out of the hanging face above Wall lake sometime in the last 36 hrs. This slab was 60 to 100cm deep and likely ran on the Jan 31 interface.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Natural avalanche activity is tapering as the snowpack slowly adjusts to the new load. However, moderate to hard sudden collapse snowpack tests today in the Bow Summit area indicate skier triggering is still very possible. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 3 natural avalanche and a skier accidental 2.5 avalanche today indicate the need for continued caution.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous soft slab and storm slab avalanches have been observed in the forecast region up to size 3. Avalanche control at roadside produced results to size 1 on heavily controlled slopes.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>