Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
The closer you are to the Cascade Crest and higher in elevation you travel, the more likely it will be to find both new and old wind slabs. The likelihood of triggering an avalanche is lower in areas further east, such as the Wenatchees. Older and deeper slabs formed on Thursday night will be less reactive, but triggering one could create an avalanche large enough to bury you.
Wind slabs typically form just below ridgelines and in gully or chute-shaped terrain features. Wind speeds have been strong, so you could encounter wind-affected snow lower down on slopes than you might expect. Look for clear signs of wind transport: dune-like drifts, cornice formation, and blowing snow. As you move about the terrain and the snow begins to feel denser and look unevenly distributed, assume wind slabs probably lurk nearby. In addition to cracking and collapsing, recent natural slab avalanches are very good reasons to avoid exposed terrain steeper than 35 degrees.
(3/18/2025)
A small sledder triggered wind slab avalanche in the Salmon La Sac (East Central). SS-AMu-R1-D1-O
Photo: Evan Pearson