Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Unlikely
- Tamaño
- 2
In the Central and Northern Bear River Range, weak, faceted snow from November is buried beneath a thick crust or multiple crusts and dense snow. On steep, wind-drifted slopes—especially where the crust is thin or missing—people can still trigger avalanches that may propagate widely. Collapsing, shooting cracks, and whumpfs, are clear warning signs of unstable snow. Remotely triggered avalanches are also possible where the overlying slab is thinner.
Snowpit profile from the Emigration Summit Area - North Aspect - 8300'. You can see the stout crust near the surface, capping the weaker snow near the ground.