Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Moderate to strong north-westerly winds have formed wind slabs on leeward slopes. These rest on a crust that provides an excellent sliding surface for avalanches. Human-triggered avalanches are likely in alpine terrain and possible at the tree line. They are found beneath ridges and alpine convexities, as well as in lateral loading zones at the tree line. Their average thickness is 20 to 40 cm.