Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Recently formed slabs of wind drifted snow will continue to be reactive in the right location with a human trigger. Cohesive slabs rest over the most recent (12/21) melt-freeze crust, which may act as a good sliding surface for avalanches. Look for shooting cracks and strong over weak layering as you assess areas of wind drifted snow. Use test slopes to check how well recent slabs are bonding before venturing into bigger terrain. Avoid wind loaded slopes greater than 35 degrees if you find signs of instability or fresh avalanches. Slabs will be deeper and wider in higher elevation terrain and near ridgelines. When in doubt, seek out wind-sheltered slopes and terrain less than 35 degrees.
Example photo of a wind slab running on a crust.