Wind Slabs
N
NE
E
SE
S
SW
W
NW
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–3
Large buried surface hoar should prolong the reactivity of recently formed wind slabs. In less wind affected areas, recent low density accumulations have been reacting as a loose dry avalanche problem in steep terrain.