Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–1.5
Snowfall and wind drifting in early December formed slabs up to a couple feet thick over facets near the ground. These weak layers are most widespread on the northern half of the compass and exist as collapsible crusts on some high-elevation southeast slopes. In the Southeast Mountains, most slabs have decayed, and the threat lingers on a few heavily drifted slopes near and above treeline. Stay alert for isolated instabilities and consider avoiding old stiff drifts above high-consequence terrain. Most lingering instabilities are expected to be small (D1-D1.5), with potential for a larger outlier on the largest, most wind-drifted slopes.
A skier triggered persistent slab avalanche on Sunday, 12/14.
East aspect of Cinnamon Mountain.