Wind Slabs
N
NE
E
SE
S
SW
W
NW
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–3
Winds have formed windslabs on lee aspects below ridgecrests above treeline. These slabs are roughly 10-15cm thick sitting on previous crusts. It is possible to initiate from skier traffic where its bonded poorly to the underlying crust.