Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Weak layers of snow formed in November are buried 2-3 feet deep beneath hard slabs. These weak layers exist on most aspects above 9000’ and any shady aspect at lower elevations on Togwotee. An avalanche was triggered three days ago on Barber’s Point involving these weak layers. It was triggered in very steep, north-facing terrain that was wind-loaded, highlighting where this problem is most likely. Remote triggering from gentle terrain above, below, or beside steep slopes is still possible. Shooting cracks and audible collapses are obvious signs of instability, but may not be present before triggering a large avalanche.
(12/10/2025)
The recently triggered avalanche on Barber's Point. This avalanche failed on weak snow formed in November.
Photo: Bridger-Teton Avalanche Center