Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Recently formed wind slabs may remain reactive to human triggers on steep and/or convex slopes; especially where they are sitting on a slippery sun crust or a weak layer of surface hoar.
Cornices are very large in many areas. Cornice failures may trigger large avalanches on the slopes below.