Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Slabs formed by strong winds during recent snowfall lie upon crusts and faceted snow that was buried on December 5th. This weak layer is widespread at the upper elevations and reaches into the upper portion of mid elevations on west through north to east aspects. Although these slabs have become less reactive, they could still be human triggered in very steep terrain with average slab depths of one to two feet.