Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
There are still some windslabs out there that developed during the last storm. They will likely be stubborn and resistant to triggering. Suspect areas will be steep terrain near ridgeline, cross-loaded gullies and convex terrain features at upper elevations. If you are seeing cracks in the surface of the snowpack or feel the snow increasing in density then you are likely on a wind slab.