Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Increasing winds are forming thin wind drifts that will be sensitive to human triggers at higher elevations. Look for blowing snow or cracking underfoot to identify the problem. There's a rare chance that you can still trigger a thicker and older wind slab that formed during last week's extreme southwest wind event, in the same type of terrain: below ridgelines, rollovers, and in cross-loaded gullies. You can avoid the problem in wind-protected or wind-eroded slopes.
This recent wind slab on Mt. Baldy exemplifies the expected size and type of terrain of most wind slabs today.