Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 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.