Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–3
Yesterday (Wednesday), riders in the Flathead Range intentionally triggered a large slab avalanche from the ridge above and noted a cycle of large natural avalanches. This continues a streak of instability (shooting cracks, collapses, avalanches) that started January 30th. The culprit is a weak layer of facets and/or surface hoar buried around a crust. Weak layers have been observed on all aspects, but the hotspot for recent activity has been on slopes facing north and east.
Steep slopes with 8+ inches of snow above the weak layer will present the greatest danger. On previously wind-affected slopes, the slab may be firm enough to support the weight of a rider. Hard slabs deserve an extra level of caution. They may not give obvious signs of instability before failing and can break widely across the slope or well above you. Sustained warm temperatures can cause liquid water to move through the snowpack and further weaken these problematic layers.
Avalanches on this layer have been remotely-triggered from nearby low-angle slopes. In today’s heat, cornice falls or remote triggers could pull avalanches farther back onto ridges than you might expect. The prudent move is to stay off of and out from under steep slopes, and give ridgelines a wide margin.
(2/4/2026)
The crown of a human-triggered, slab avalanche in the Flathead Range. The rider triggered the slide from the ridge on a buried layer of surface hoar. It propagated widely (1000ft) and ran 700ft into the flats below.
Photo: Michael Reavis