Storm Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
Around 30 cm of recent snow overlies various layers formed mid-November, including surface hoar, faceted grains, and a hard crust. The recent snow may not bond well to these layers.
Wind may have redistributed the storm snow at high elevations, forming isolated wind slabs in lee terrain features.
Avalanche hazard is unlikely anywhere snowpack depths have yet to overcome ground roughness like brush and rocks.