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</style><p class="p_CC664AAA"><span class="s_3FE45715">The region picked up 5 - 10cm of convective snowfall Saturday night which adds to the 60 - 100 cm of storm snow fell in the last week. Winds have been out of the SW through NW which has created fresh wind slabs in lee terrain. Around 70 cm of settling storm snow rests on a graupel layer that can be found in much of the region. This makes for around 90 cm on top of the mid march crust at this point. This crust exists on all aspects below 2000m and on solar aspects in the high alpine. North of Sparwood and in the Crowsnest Pass area, the buried crust seems more specific to previously sun-exposed slopes. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The deep mid-February facet/crust persistent weakness, now down up to 150cm, seems unlikely to trigger in areas where the hard, supportive crust exists. No matter where you are in the region, this weakness should stay on your radar as any activity at this interface would be large and destructive. Possible triggers include a large cornice fall, a large input in a thin snowpack area or solar warming. Cornices are also large and unstable.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">See this </span><a href="https://www.youtube.com/watch?v=2FilGUG0Fk4" target="_blank"><span class="s_B5813F7D">great video</span></a><span class="s_3FE45715"> from our South Rockies field team that does an awesome job of summarizing the current state of the snowpack.</span></p>