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</style><p class="p_CC664AAA"><span class="s_3FE45715">Tuesday there were several reports of skier triggered wind slab avalanches up to size 1.5 on a variety of aspects between 1800-2100 m, including a remotely triggered (from a distance) pocket of hard wind slab near ridge top. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural wind slab avalanches to size 2.5 were reported on a south / west through north / west aspects between 1800m and 2400m.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, natural wind slab activity was widespread above 1900m on primarily south east through west aspects. We received reports of an initial wind slab (size 2) stepping down to deeper weak layers and triggering a size 3.5 persistent slab, on a south west aspect near 2300m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Also on Sunday, skiers were able to trigger small storm slabs low down on MacPherson on the widespread rain crust that formed February 8th. </span><a id='GoToAdded' href="http://www.avalanche.ca/mountain-information-network/submissions/21274985-cb61-402a-8397-303fee59a6f0" target="_blank"><span class="s_B5813F7D">See the MIN report for more details.</span></a><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Although deeper, persistent avalanche activity has become less frequent over the past week, light triggers in shallow rocky areas, as well as large triggers such as a cornice collapse or step down from a wind slab release, still have the potential to result in large destructive avalanches.</span></p>