Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Managing our persistent slab problem has become more difficult following our most recent storm cycle. In areas with a deeper snowpack (Mammoth – June), signs of instability may be hard to find. Large slope scale collapses and long shooting cracks continue to be reported in areas with more shallow coverage. In either scenario, a resulting avalanche will likely involve the full depth of the snowpack and may be unsurvivable. While triggering a large persistent slab avalanche will be easier in areas with a generally shallow snowpack, shallowly buried rocks, trees, and convex rollovers will act as good trigger points in areas with a deeper snowpack. These avalanches can be triggered remotely from adjacent terrain and may propagate long distances and beyond terrain features that typically contain surface instabilities like storm or wind slabs. Avoiding overhead hazards and sticking to slopes less than 30º can help you manage this problem today.
Photo: Steve Mace
large persistent slab avalanche activity in the June BC