Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–2.5
While unlikely, we can't write off triggering large avalanches in middle and upper elevation terrain while the snow keeps piling up. Unfortunately, you probably won't receive any obvious signs of instability before triggering one of these lingering monsters. We are most concerned with a layer of weak facets found near the ground on middle and upper elevation slopes, especially those facing away from the sun.
Triggering a slide on this layer is most likely in rocky, heavily wind-affected areas where the snowpack depth is variable, and in more sheltered terrain where the snowpack is around 3 feet deep. Smaller wind slab avalanches or sluffs (Problem 1 above) could "step-down" as they travel down slope, triggering much larger Persistent Slab avalanches.
(12/30/2025) Large avalanche in Wilson Ck and another on Duncan Ridge. Photo: Sawtooth Avalanche Center