Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
New snow and wind has formed wind slabs in lee terrain features at treeline and above. Wind slabs are forming over old wind affected surfaces and/or melt freeze crusts. Recent wind slab avalanches are running fast and far on a crust.