Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2.5–3.5
Intense periods of precipitation have the potential to bring buried weak layers to their breaking point. A layer of buried surface hoar and facets that formed in late November and a widespread facet/crust layer from early November have the potential to become sliding surfaces with the stress of the new snow and rain. Easy-to-trigger wet loose or storm slab avalanches have the potential to step-down to these deeper layers and produce large, destructive avalanches.