Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1
At the upper elevations winds that veered from the south to the west-northwest have formed dense pockets of new wind slab. These slabs lie upon sun crusts and firm old snow surfaces. They could be human triggered in steep wind loaded avalanche starting zones, on steep rollovers and in cliff areas with depths to one foot.