Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind blown snow in catchment areas, gullys, below ridgelines has formed slabs of more dense over less dense snow. In some areas a combination of sugary faceted snow and crusts are underneath these more dense slabs. Snow surface cracks and hollow sounding snow are signs of wind slab. Also look for textured surfaces on leeward slopes below or adjacent to ridgelines. Avoid wind slabs in steep terrain and above terrain traps.