Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 2
The underlying snow pack is weak, but the December drought layer (buried roughly 15 inches deep) is the primary layer of concern. This layer of weak, faceted snow formed near the surface during the December dry spell. A slab now exists on top of this persistent weak layer. Near treeline and below, storm snow over the past week has settled into a thick, cohesive slab. Near treeline and above, elevated winds have stiffened the snow and produced slabs of wind drifted snow over top of this weak layer. In our travels on Thursday, we experienced collapsing and whumphing. These red flag signs of instability are the effects of a person's weight collapsing a slab on a weak layer. The video below of an extended column test illustrates the slab's ability to propagate and produce an avalanche: