Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
The new snow overlays a buried persistent weak layer (PWL). This weak layer consists of surface hoar, facets and/or a suncrust. The storm snow has overloaded this PWL, producing large avalanches where it is present in the start zone or within the track of the path.