Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
Incremental snowfall and recent strong winds formed reactive wind slabs in the alpine and open areas at treeline that remain possible to human-trigger. If triggered, wind slabs have the potential to step-down to deeper weak layers. This problem also overlaps with where cornices may be reaching their breaking point.