Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Unlikely
- Taille
- 2
While there is little soft snow available to drift, in steep terrain at upper elevations, people should watch for and avoid stiff drifts or wind slabs formed by redeposition on a widespread layer of weak surface snow consisting of near-surface facets or surface hoar. The surface snow continues to weaken, and small loose avalanches of sugary, faceted snow are increasingly possible on very steep slopes.