Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely - Possible
- Size
- 1.5–2.5
The bottom of the snowpack is weak, comprising facets and depth hoar. Recent warm temperatures and winds have promoted slab development in the mid and upper snowpack. Use caution with steep or planar slopes where failures of these slabs may be more likely to propagate.