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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+/- of storm snow has been redistributed by moderate S'ly winds near ridgecrests in the alpine and exposed treeline. Below these slabs, the Feb 22nd persistent weak layer is now buried down 60-90cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. In some locations, this surface hoar sits on a crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface snow is moist on solar aspects during the heat of the day. 20cm settling storm snow is being blown into windslabs by moderate SW winds, with windward ridgetops in the alpine stripped to rock. This sits on previous windslabs and crusts. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices are large and looming.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the alpine the wind is starting to produce soft slabs in lee areas. New sun crusts exist on steep solar aspects. 40-50 cm of recent snow sits over the Feb 29 crust interface on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base, while thick areas have a stronger base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds on Tues and overnight Wed will have blown snow and created small windslabs directly beside ridge crests that are prone to human triggers. In some areas, this snow overlies buried sun crusts formed in late February. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme SW winds transporting available fetch to outer space and lee aspects forming new windslab low in start zones. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weak and shallow; bridging over the basal weakness is less reliable BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+/- of storm snow has been redistributed by moderate southerly winds creating soft slabs in exposed areas. Below these slabs, the February 22nd persistent weak layer is now buried down 60-90cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. 15cm of storm snow is expected to fall today. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds on Tues and overnight Wed will have blown snow and created small windslabs directly beside ridge crests that are prone to human triggers. In some areas, this snow overlies buried sun crusts formed in late February. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow is bonding well to older snow surfaces. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weak and shallow; bridging over the basal weakness is less reliable BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-30cm of snow and mod/strong SW winds last night has created a reactive storm slab. The new snow sits on a thin suncrust on solar aspects and small surface hoar on N'ly aspects. Below this slab, the Feb 22nd persistent weak layer is down 80-120cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow over the last 2 days has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> The Icefields area has a well bridged midpack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack above the basal facets and depth hoar.The fridge air will make for weak bonding of the new snowfall.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> Sun crusts are largely absent and the melt is evident in the valley bottom with rocks starting to appear. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-30cm of snow and mod/strong SW winds in the last 48hrs has created a reactive storm slab. The new snow sits on a thin suncrust on solar aspects and small surface hoar on N'ly aspects. Below this slab, the Feb 22nd persistent weak layer is down 80-120cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Up to 20cm of new snow from convective flurries yesterday overlies wind affected surfaces including windslab and crusts from the extreme wind event earlier in the week. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices are large and looming. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow over the last 3 days has been redistributed by moderate winds of variable direction at treeline and above creating wind slabs in open areas. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The Icefields area has a well bridged mid pack overlying basal facets and depth hoar.  3-5 cms new snow from pm Mar 12th blanketing Hs. The northern region is weaker with less bridging  midpack strength above basals and depth hoar.  Isolated strong NE valley winds in the townsite area stripping existing snowpack and reverse loading Alp/TL features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of storm snow on Tues night, that came in with mod to strong SW wind, is now settling over the Mar 10 interface of surface hoar on shaded slopes and suncrust elsewhere. Below this slab the Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> 15-25cm of snow over the last 3 days has been redistributed by moderate winds of variable direction at treeline and above creating wind slabs in open areas. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust is present. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds past 36 hrs stripping and redistributing upper snowpack. Wide spread scouring in exposed places. Hard slabs, soft slabs, sastrugi now present. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds are building fresh windslabs in unusual places. The Mar. 10th interface of suncrust on all solar aspects and possibly small surface hoar on shaded slopes, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust is present. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. On some steep solar aspects a thin sun crust is present. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A variety of wind affected surfaces. Wide spread scouring, stripping in exposed places. Hard slabs, soft slabs, sastrugi now present. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds Friday-Saturday built windslabs in unusual places. The Mar. 10th interface of suncrust on all solar aspects and small surface hoar on shaded slopes, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust may be present. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread scouring, stripping in exposed places. Hard slabs and sastrugi now present. Sun Crust on S-SW aspects to ALP and Temperature crust on E-SW aspects TL and below. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most open terrain is heavily wind effected from the strong NE winds Friday-Saturday. The Mar. 10th interface of a suncrust on all solar aspects, and isolated surface hoar, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A sun crust is developing on the surface. Waterton received 40cm of snow in the townsite &amp; 20cm at Cameron Lake over the weekend. This storm was accompanied by easterly winds so expect </span><a href="https://www.avalanche.ca/glossary?q=rev#reverse-loading" target="_blank"><span class="s_9255B882">reverse loading</span></a><span class="s_AA239A9B">. The new snow is settling fast thanks to high daytime temperatures. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, Surprisingly little activity noted recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong diurnal temperature swings have built a crust on solar aspects that will break down with daytime warming. Open terrain at upper elevations is heavily wind effected from the strong NE winds Friday-Saturday. The Feb 22 PWL is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. Widespread wind effect in the alpine from recent multidirectional winds with 5 cm new snow on top. On sheltered Northerly aspects there is 15-20 cm over a firm mid-pack.  In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold nights and warm days have built a crust on slopes facing the sun. Expect this crust to break down with daytime warming. Open slopes at upper elevations are very wind effected from the strong NE winds Fri-Saturday. The Feb 22 PWL is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. Widespread wind effect in the alpine from recent multidirectional winds with 5 cm new snow on top. On sheltered Northerly aspects there is 15-20 cm over a firm mid-pack. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts have formed on slopes facing the sun. These crusts will break down with daytime warming. Open terrain treeline and above has widespread wind effect from strong weekend winds. Cool overnight temperatures are starting to facet upper snowpack. The dormant Feb 22 surface hoar and crust combo is down 90-130cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5cm of recent snow distributed by L NE winds overlies a thick MFcr on solar aspects. North Faces are generally wind affected from previous strong northwest through northeast winds. The midpack is strong and well settled, though basal weaknesses exist in thinner snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow that fell Wednesday now has a suncrust on solar aspects. Widespread wind effect in the alpine from recent multidirectional winds. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface has been affected by intense sun and the freezing level rising to at least 1900m yesterday. At treeline and above exposed terrain was heavily affected by the wind last weekend and varies from impenetrable to skis to punchy in places, especially where facetted by overnight cold temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow that fell Wednesday now has a suncrust on solar aspects. Widespread wind effect in the alpine from recent multidirectional winds. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A supportive Melt freeze crust now exists on all Solar aspects to Alpine elevation. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface has been affected by intense sun and the freezing level rising to at least 2100m yesterday. At treeline and above exposed terrain was heavily affected by the wind last weekend and varies from impenetrable to skis to punchy in places, especially where facetted by overnight cold temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation Wednesday. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-5 cm of new snow in eastern areas of the forecast region on Saturday night. Widespread wind effect in the alpine and down into treeline. Sun crusts on solar aspects and buried sun crusts on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak faceted base, while deep snowpack areas have a solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasted snow (up to 5-8cm overnight Sunday) over a supportive melt freeze crust exists on all Solar aspects to Alpine elevation. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface crusts exist on all aspects to 1300m and on SE-W into the alpine. Surface hoar has been developing over the last few nights to 3mm with shady sheltered pockets in the trees up to 10mm. Wind affected surfaces in exposed tree line and the alpine vary from impenetrable to skis to punchy in places.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread wind effect in the alpine and down into treeline. Sun crusts on solar aspects and buried sun crusts on steep solar aspects. In most areas of the Little Yoho region a deep snowpack exists with few weaknesses, though thin areas still have a weak facetted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-10 cm of snow on Monday with the higher amounts in the west. Moderate SW winds in the alpine forming new wind slabs. Previous widespread wind effect in the alpine and treeline. Sun crusts and buried sun crusts on solar aspects. In thin snow pack areas a dense mid-pack sits over a weak faceted base, while deep snowpack areas have a solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Traces of new snow overnight on a supportive melt freeze crust exists on all aspects, BTL and solar aspects at TL and Alp elevations. Snowpack has yet to have a deep melt freeze cycle and basil weakness is still a looming hazard sensitive to large loads like your mum, and cornices.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface crusts exist on all aspects to 1300m and on SE-W into the alpine. Surface hoar has been developing over the last few nights to 3mm with shady sheltered pockets in the trees up to 10mm. Wind affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A supportive crust exists on the surface that will be buried by incoming snow. The exception is straight north facing slopes where new snow will fall on settled powder in sheltered areas, and wind slabs everywhere else. The mid pack is strong and well settled. Basal instabilities haven't been seen in some time, but are likely lurking in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-10 cm of snow at upper elevations on Monday. Moderate SW winds in the alpine forming new wind slabs. Previous widespread wind effect in the alpine and treeline. Sun crusts and buried sun crusts on solar aspects. In most areas of the Little Yoho region a deep snowpack exists with few weaknesses, though thin areas still have a weak facetted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moist new snow, more in the front ranges on a supportive melt freeze crust exists on all aspects, BTL and solar aspects at TL and Alp elevations. Snowpack has yet to have a deep melt freeze cycle and basil weakness is still a looming hazard sensitive to large loads like cornices.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of storm snow overlies a crust on solar aspects (SE through W) into the alpine. The new snow sits on surface hoar on shaded, polar aspects. Previously wind-affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The mid snowpack is consolidating providing good bridging strength over the weak base. Sun and temperatures crusts laminate the upper snowpack. At treeline and above watch for thin windslabs over these crusts where bonding may be poor, particularly on solar facing slopes. Cornices loom large and are particularly capricious at this time of year. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of storm snow overlies a crust on solar aspects (SE through W) into the alpine. The new snow sits on surface hoar on shaded, polar aspects. Previously wind-affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of storm snow has been redistributed by Moderate - Strong SW winds. This has created fresh windslabs which sit over a melt freeze crust on all but North aspects. The mid pack is strong and well settled. Basal instabilities haven't been seen in some time, but are likely lurking in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>