Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Currently, you could find stubborn older slabs just below ridgelines or in cross-loaded gullies and couloirs. Smaller but more recently developed slabs may have formed over surface hoar. Hazard will increase if new snow falls and is blown around by the wind. Anticipate new slab development on lee slopes if you see blowing snow. Hard, uneven snow surfaces, rapid changes in snow depth, and cornices indicate that terrain has seen previous snow transport. Surface hoar often appears as a thin grey line in a snowpit wall; you can dig a quick hand pit to check for it. Signs of instability include shooting cracks, collapsing, and recent slab avalanches
(12/31/2024)
Cornice fall triggered a small 1ft deep wind slab avalanche in the East South zone recently.
Photo: Payton Schiff