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. Unfortunately, you may not receive any obvious signs of instability before triggering one of these lingering monsters. We are most concerned with deeply buried 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 on steep windy and/or rocky slopes where the snowpack depth is variable and in more sheltered terrain where the snowpack is around 3 feet deep.
Additional Discussion: You may be able to trigger wind slab avalanches that formed near ridgelines and in cross-loaded areas on the sides of gullies. Look for recent cornice growth, dunes, or ripples in the snow surface and listen for hollow-drum-like sounds as indicators that you've found wind slabs. These may break wider than expected due to crust interfaces in the upper snowpack.
(12/28/2025) Large natural avalanches. Paradise Peak and West Fork Big Creek. Photo: Sawtooth Avalanche Center