Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Recent warming and wind have formed a surface slab that caps a weak layer (facets or surface hoar) and crusts on multiple slopes. Observers report shooting cracks, poor snowpit test scores, and a remotely triggered slide (See adjacent image). The weak layer is found within the top foot of the surface in sheltered locations and buried 2 to 3 feet deep on wind-loaded slopes.
Slides can be triggered remotely from flat terrain above, to the side, and below steep slopes.
Look and feel for dense surface snow where your skis, board, or machine do not sink in as deeply. Cracks beneath you indicate you have found a slab, while cracks shooting away from you indicate a sensitive slab. This is a near-surface problem, and hand pits are a good way to confirm the presence of surface hoar.
Seek out softer snow and low-angle slopes for a safer and more enjoyable experience.
Storm or Wind Slab: The Flathead Range was favored with up to 5 inches of dense snow recorded at the Tunnel Ridge snow station. Riders may encounter slab-like conditions in the new snow. Expect to find up to a foot of drifted snow on the leeward slopes that may be reactive to your weight. A triggered slide in the new snow may initiate an avalanche on a buried weak layer, resulting in a larger slide.
(1/31/2026) This small soft slab avalanche was triggered by a motorized rider in the northern Whitefish Range on Saturday. This likely failed on the buried weak snow + crust setup. Riders could trigger slides similar to, or larger than, this one today.