Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–2
Cohesive surface slabs formed by recent warming and/or wind may sit over a crust and weak surface hoar or facets. This is most problematic in areas where greater amounts (>20 cm) of recent snow have accumulated over the weak layer.