Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely - Possible
- Size
- 1.5–2.5
The new snow overlays a buried persistent weak layer (PWL) that consists on suncrust, facets and/or surface hoar in some locations. Warm temps are promoting the settling of a cohesive, reactive slab on top of this layer. Expect this slab to become more reactive during times of intense solar.