Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Two persistent weak layers exist in the snowpack. The upper layer is down 30-50 cm and consists primarily of facets. The deeper layer is down 60-100 cm. This layer consists of surface hoar, facets, and/or a crust. The problem has been most prevalent around treeline and in openings below treeline, but also reaches into the lower alpine.
In areas where the snow is dry (soft or wind-affected), or where a breakable crust exists, it may still be possible to trigger a persistent slab.