Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Persistent weak layers exist in the upper snowpack and near the bottom. Snowfall and wind today could increase the sensitivity of the problem. Wind-drifted slopes are the most dangerous as they will receive the most loading. Weak layers in the upper snowpack have been quiet in the Southeast Mountains due to less recent snowfall, but this storm may help increase the distribution of slabs near the surface in wind-sheltered areas. The safest way to manage this problem is by avoiding heavily drifted slopes and terrain with highly variable depths to reduce the chance of finding a trigger point. Avalanches that fail near the bottom of the snowpack would be hard to survive, and avalanches that break in the upper snowpack could be large enough to bury you.
Examples of recent Persistent Slab avalanches from the Northwest Mountains. This type of activity could spread into the Southeast Mountains during this storm.
(3/16/2025) Photo: Crested Butte Avalanche Center