Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2
Several weak layers are buried in the upper 1-2.5 feet of the snowpack. On slopes that face away from the sun, you'll find some surface hoar and facets at these interfaces. On slopes that face the sun, you'll find crusts with some small facets here. Moderate to strong winds this week created a batch of stiff wind drifts in terrain exposed to the wind, building slabs on top of these buried weak layers. Thursday, skiers on Titus Ridge found this combination of unstable slab+weak layer when they remotely triggered a small wind slab from 50 feet away (photo here). Wednesday, a wind slab released naturally on Della Mountains, west of Hailey (photo here). Cracks shooting out from your machine or skis are clear indicators of an unstable slab. Small slabs that knock you off your feet and send you downslope can have high consequences in the wrong terrain.
Further down in the snowpack, you'll find layers of weak snow near the ground. Triggering an avalanche on these layers is most likely in wind-affected alpine terrain where scouring has produced thinner areas of the snowpack. Here, you'll have better access to this weak snow and triggering a slide involving it remains possible.
Avalanches failing on persistent weak layers can break well above you on the slope and may break wider than you expect. You can significantly reduce your risk by steering clear of wind-affected, rocky, alpine terrain steeper than about 35 degrees.