Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
Beneath the thick surface crust in the Central and Northern Bear River Range, weak, faceted snow from November is buried under heavy, dense snow one to two feet deep. In isolated previously drifted areas where the crust is thinner or not present, human-triggered avalanches remain possible and could propagate widely across a slope. Remotely triggered avalanches failing on a persistent weak layer are possible.
- Even small avalanches can have serious consequences in shallow snow conditions, as you might be dragged through the rocks or downed trees below.
- Follow safe travel protocols: travel with a partner, cross (or ride) steep slopes one person at a time while the rest of your party watches from a safe place.
A bombproof crust locks up the shallow snow in the Tony Grove Area.