Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Weak snow exists 1-2 feet below the snow surface. This layer is composed of surface hoar and near-surface facets from our prolonged high-pressure spell. Though becoming less likely, you are most likely to encounter this problem on shaded slopes facing NW-N-NE above 6,500 feet. Be heads-up around steep slopes that have been protected from the sun and wind, such as terrain features similar to those shown in the photo on the right. Persistent slab avalanches are becoming difficult to trigger. As more time has passed since the last major storm, it is unlikely that there will be any clear feedback (such as cracking, collapsing, or whumpfing) before an avalanche. The weight of a snowmachine is much more likely to affect buried weak layers than a person's weight.
The most sensitive slopes are at mid-elevations. These could likely be small terrain traps that catch riders off guard, such as this one that claimed a life in early January in western Wyoming. Don't let your guard down when persistent slab avalanches are on the menu. Your best tools for managing this problem are safe travel practices, including traveling one at a time in avalanche terrain, keeping an eye on all members of your party, and digging into the snowpack to perform a snowpack test or check for weak snow at the depths mentioned.
ADDITIONAL DISCUSSION: Watch for small surface slabs of new snow, 2-4 inches deep at upper elevations, formed by gusty SW winds overnight. The problem above is the more consequential issue in this zone due to less snowfall.
(2/10/2026)
Intentionally-triggered persistent slab avalanche. This failed on a layer of surface hoar two feet deep, which was buried 2/8.
Photo: Payette Avalanche Center