Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
Slabs of wind blown snow have formed in near and above treeline areas. New cornices, wind pillows, and snow surface clues may help identify where these wind slabs have formed. Snow surface cracking and/or dense snow over less dense snow may indicate unstable wind slab. Make a plan to avoid areas where unstable wind slabs may exist.
Wind slabs formed yesterday with new snow and increased winds. These wind slabs have formed on top of a variety of snow surfaces including crusts and sugary near surface facets. As these slabs consolidate and gain more strength, wind slab avalanches could continue to be triggered today on these previous old snow surfaces. Greater hazard will exist near and above 8000' where the most storm snow fell.
(2/11/2026)
A cornice kick triggered this avalanche on a wind loaded East aspect. Crown 1' deep.
Red Lake Peak, Carson Pass area.