Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
At the higher elevations stronger northwest winds during the past 24 hours have likely increased the development of wind slabs. Earlier slab formation was caused by southwest to west winds. At the higher elevations large slab avalanches could be human triggered on density breaks and firm wind-packed snow surfaces. At the mid and lower elevations soft slab avalanches could be triggered on density breaks, wind-pack, sun crust or faceted snow layers. These slabs could be 1 to 3 feet deep.