Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 1.5–3.5
There is a layer of facets/surface hoar/crust in many parts of the region down 40-110 cm. Skiers, new snow, wind, falling cornices, dry loose, or storm snow avalanches may be enough of a trigger to overload this layer.