Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Skiers and riders could trigger dense surface slabs up to two feet in depth. These slabs lie upon crusts and buried layers of faceted snow that formed in January and are unstable on steep slopes where faceted snow is well preserved or lies upon those crusts. New snow accumulations will increase the load on areas of unstable snow and increase the potential for these slabs to be triggered by humans.