Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Weak snow that formed in November sits near the base of the snowpack in the majority of terrain above 8,500’. These weak layers have been stressed from recent storms. Triggering a persistent slab avalanche is most likely in very steep terrain that faces east through north. An observation from 2 days ago included a remote trigger, cracking and collapsing. These are clear signs of an unstable snowpack. Continue to give the snowpack time to adjust from the recent storm cycles.
(12/29/2025)
This avalanche is NOT from Togwotee pass but illustrates the nature of a persistent slab avalanche failing on weak layers near the ground.
This is from the North Fork of Mosquito Creek. 8900', NE aspect, D3 3 days ago.
Photo: Bridger-Teton Avalanche Center