Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
Tuesday's storm formed slabs 1 to 2 feet thick above a widespread persistent weak layer. A natural avalanche cycle occurred on Tuesday and observers reported many avalanches large enough to bury and kill a person. The most dangerous terrain faces west through north through east as these aspects contain the thickest and most continuous weak layer however, some southerly-facing slopes also have the weak layer at upper elevations.
Due to thinner, old snow coverage prior to Tuesday's storm, fewer below-treeline slopes and fewer sunny alpine slopes hold old, weak snow in the Southeast Mountains. This means that avalanche conditions are slightly better than in Northwest Mountains as there are fewer slopes with the slab/weaker layer combination to produce avalanches below-treeline and on sunny, upper-elevation slopes. Even with this distinction, dangerous avalanche conditions exist in the Southeast Mountains.
A natural avalanche on Mount Emmons' easterly-facing terrain.