Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
Many places with enough snow to avalanche have a weak layer of basal facets and/or a melt freeze crust at the base of the snowpack. This weak layer has become less sensitive but can still be triggered by people and propgate a significant distance. Use caution in steep loaded terrain.