Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
Last weekend's snowfall and wind drifting formed slabs up to a few feet thick over facets near the ground. These weak layers are most widespread on the northern half of the compass and exist as collapsible crusts on some high-elevation southeast slopes. Shooting cracks and collapses are clear warnings, but be aware that direct feedback is decreasing with each passing day. Persistent slabs can break well above you and be triggered remotely from low-angle terrain adjacent to or below steep slopes. Previous winds often drive the location of slab formation; low-elevation terrain in sheltered areas is less likely to harbor cohesive slabs. The most reliable way to avoid the problem is terrain selection: stick to slope angles consistently less than about 30 degrees or travel on terrain that was bare ground through November.
This avalanche was remotely triggered on a small terrain feature, releasing the entire snowpack. This avalanche would pile up deeply in a terrain trap or grow larger in bigger terrain. 12/7.