Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Lingering wind slabs 1- 2 feet thick exist on lee aspects at upper elevations. These slabs will be isolated to very steep terrain, directly below exposed ridgelines, or in cross-loaded terrain features. There is a chance these slabs could break deeper than expected in areas around rocky unsupported slopes and convexities. Look for pillows, drifts, and cornices to identify where these slabs may have formed.
It’s unlikely you’ll trigger a very large avalanche that fails on deeper weak layers buried up to 3 feet at middle and upper elevations. At lower elevations where the snowpack is thinner and temperatures are warmer, avalanches involving these layers will be possible. This layer can be found in pits and is still showing propagation in tests, but is deep and less likely to be impacted. While the likelihood is decreasing, the consequences of triggering a very large avalanche on this layer remain high.
Multiple tracks on a slope do not indicate stability. The best way to manage this problem is to give yourself a safety margin around terrain traps and rocky, convex, very steep slopes today.
(2/11/2025)
This layer of concern now has another 3 feet of snow loading it...
Photo: Bridger-Teton Avalanche Center