Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1.5–2.5
Weak snow from November forms the base of the snowpack on many slopes here. The slab over this weak snow has been building in December and is now 2-3 feet thick. Avalanches failing on this layer will easily be large enough to bury you. Slabs may break wider than you expect, wrapping around terrain features. Triggering slides remotely — from a distance away from the slope that avalanches — is a real possibility.
This layer is at its worst on upper elevation slopes and middle elevation slopes that face away from the sun (W-NW-N-NE-E). Here, a pile of facets is resting on top of a stiff, icy, crust. This combination produced a number of avalanches during loading events and has not had time to gain significant strength. The slab over the weak layer has grown thick enough that it keeps us above the weak layer in places. However, if you are able to collapse the weak layer, the avalanche you create will not be small.
Yesterday, I experienced 6-8 deep collapses while traveling at middle and upper elevations in this zone. This clear indicator of instability, combined with the unstable test scores I received on this layer in 3 different snowpits, was more than enough evidence to have me avoiding steep avalanche terrain where this layer exists.