Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Certain
- Size
- 1.5–2
Large, 1-3’ thick avalanches are almost certain. Storm snow is perched precariously atop well-developed weak layers, including facets, facet + crust combinations, and surface hoar (image). Snowfall and continued wind-blown snow will push many slopes to their breaking point.
While the size and likelihood of these slides increase in areas exposed to the wind—all steep slopes are suspect. Cracks shooting out from your skis or boards clearly indicate instability. Avalanches can be triggered from a large distance above, below, or to the side of the slope that avalanches.
These smaller Persistent Slab avalanches could "step down," triggering the much larger avalanches described below.
(1/11/2024) This large avalanche was remotely triggered in the Headwaters drainage. Ben and his partner on Thursday afternoon were over 100 feet away, on the opposite side of the ridge when they triggered this collapse and resulting avalanche. This avalanche ran through some very hazardous terrain and was plenty large to bury a person.