Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible - Likely
- Tamaño
- 2–3
A weak layer that formed as a crust in mid-November persists in the region. This layer may wake as rapid loading from new snow, wind, or smaller storm slab avalanches stresses deeper instabilities, resulting in larger and more destructive avalanches.