Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Strong winds from the southwest have created fresh wind slabs in and above the treeline today. These slabs are the most sensitive in localized terrain features such as convexities and start zones. Under the fresh slab snow exists a stout melt freeze crust 12" or more below the surface. This crust is a likely sliding layer for the slab. Wind-driven snow shows its clues on the surface and it can also be felt under the ski or foot.