Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Past snowfall was transported by winds that veered from the southwest to northeast and formed into slabs. These slabs lie on a variety of aspects at the high elevations and could be released by the weight of a single person with one to two foot depths. These slabs can be found in very steep rocky areas and will generally have the appearance of a wind loaded feature.