Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Ongoing and previous wind loading, including cross-loading, has created wind slabs of varying size and distribution on all aspects. Larger, denser, and more reactive slabs reside primarily on east aspects. Slabs will be most common just below ridgelines, in cross-loaded gullies, on concave terrain, and around rock outcrops. Wind-textured or lens-shaped snow surfaces are key indicators of a wind-loaded slope. Use snow and terrain observations to identify areas of concern, heed red flags, and favor mellow, wind-sheltered, or windward slopes to reduce your risk.
This photo was taken from last season but highlights all the “watch-outs” to observe for today: snow transport, cornices, and surface texture.
Photo: Eric Falconer