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
Some of these have occurred due to reverse loading, from northerly winds. Slabs up to 30cm have been formed in the immediate lee of ridgelines.