Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
New snow will drift into reactive soft and hard slabs across exposed middle and upper elevation terrain. These slabs may not be that thick, but they could be easy to trigger and propagate wider than you may expect if they form over weak snow surfaces from the recent high pressure.
These wind slabs will be most prevalent on the downwind sides of ridges, below cornices, and beneath rock bands. Look for blowing snow, dune-like drifts, and sharp cornices to help you identify what slopes are loading up. Stiff snow surfaces and cracks shooting out from your feet or machine are obvious clues that you found a slab. You can reduce your exposure to this problem by sticking to ridges and slopes under 30 degrees.
If you find over 6 inches of new snow, it may be possible to trigger shallow storm slabs in more wind-sheltered terrain. Carefully assess the new/old snow interface before committing to steep slopes.
(3/14/2025)
Blowing snow and drifted ridgelines are good indicators that reactive wind slabs may exist on the slopes below.
Photo: Joe Dellaporta