Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
A widespread, well-preserved buried weak layer was responsible for multiple natural avalanches in the Flathead Range this week during the recent near-record warmth. This layer lies within the top foot or so of the surface in sheltered terrain and around two feet deep on wind-loaded slopes.
The recent heat wave has stiffened surface snow into a cohesive slab on polar aspects and a crust of varying strength on sunny slopes. You may not notice signs of instability, such as cracking or collapsing, before triggering a slide. This problem is notorious for riders remotely triggering avalanches from flat terrain above, to the side, and below steep slopes.
This is a near-surface problem, and hand pits are a useful tool for confirming the presence of a buried weak layer.
Sticking to a supportable crust will minimize the risk of impacting the weak layer. Choose low-angle slopes that are not connected to steep slopes in areas without a crust.
Wet Loose: Today's forecasted rain may wet previously dry snow, resulting in small wet loose slides. If the freezing line rises higher than expected, this problem will become more widespread.
(2/6/2026) This is a large natural slab avalanche near the Great Northern Mountain. This occurred during the recent warming and likely failed on a buried weak layer.