Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2.5
Weak layers of faceted snow and surface hoar are buried 1 to 3 feet deep. You are most likely to trigger a slab avalanche where recent snowfall has been stiffened by wind or sun. You might see or feel obvious signs of cohesive slabs at the surface (i.e. wind-textured snow, or cracking). In some locations, slabs are covered by recent low-density snow. Probing or digging are reliable methods to confirm if a slab has formed.
Today's increasing southwest winds will continue to load weak layers while building thin surface slabs. Steer away from likely trigger points like convex roll-overs or slopes peppered with rocks. Natural and human triggered avalanches occured during the last 3 days in zones north and south of the advisory area. Observations from the Whitefish Range continue to feature buried surface hoar and obvious signs of instability like "whumpfing" collapses.
(2/13/2025) D1.5 slide triggered on eastern aspect at 6600ft. 35 degree slope angle.