Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind Slabs that formed over the weekend may still be lingering near ridgelines, the base of cliffs, in confined gullies, or on convex features. These slabs were formed by atypical east winds, so they could exist on different features or aspects than you are used to. Look for large “pillow-like” piles of snow, fresh drifts behind objects, or small freshly built cornices to help you identify where wind-loading has occurred.
(12/3/2022)
This skier-triggered slab in the Alpental Valley caught and carried an individual for a short distance on 12/3. No burial or injuries were reported. [Bryant Peak Couloir]
Photo: Public Observation