Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Increasing southwest winds and light snowfall may form thin slabs of wind-drifted snow on leeward slopes later today. Slab development will depend on the arrival and quantity of new snow. These features are found downwind of ridgelines, saddles, tree stands, and rock outcroppings. Sidewalls of cross-loaded gullies can accumulate substantial drifted snow.
Blowing snow points in the direction of fresh slab development. Dune-shaped or pillow-like features identify areas of wind-drifted snow. Cracking in the snow surface indicates instability directing you to lower-angle or terrain sheltered from the wind.
(12/2/2024)
This is an example of a small wind slab at a mid-slope location. Slabs tend to be larger and more dangerous near ridgeline elevations.
Photo: Flathead Avalanche Center