Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–2.5
Weak layers are persisting in the snowpack beneath hard slabs 3-5 feet deep. These layers are trending dormant without any stress from rapidly changing conditions. There are a lot of slopes where this problem is unlikely. Thin spots (trigger points) where the overlying slab is shallow and riders can impact these weak layers are most common in steep, rocky, unsupported and wind affected terrain. Be mindful if traveling in terrain with those characteristics. Using your probe to check for thin, shallow slabs above weak snow can help you gain a better understanding of the slopes where you should remain suspect.
The last avalanche involving persistent weak layers was triggered by a large cornice fall on 2/21. The last human triggered avalanche on these layers occurred on 2/10.
(2/17/2024) Photo: Teton County SAR
A very large persistent slab avalanche that occurred on No Name Peak after a period of significant loading.