Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 2–3.5
Previous to the incoming storm snow, a buried persistent weak layer has been observed throughout the region 30 to 80 cm below the surface. The catch is that this layer is present on some slopes, and then absent on nearby slopes. This storm is likely to initiate a natural avalanche cycle that could easily trigger very large persistent slab avalanches. It will be a good test in the long run, but this is a time to avoid avalanche terrain while the snowpack tries to sort itself out.