Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible - Likely
- Taille
- 1–2
Recent wind slabs rest on the crust formed after the thaw. On certain slopes, a layer of faceted grains has formed above this crust, creating an excellent sliding layer. This combination of grains is not found everywhere, so it is important to carefully assess the slope before skiing.