Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
On steep slopes that haven't already avalanched, you can easily trigger persistent slabs over buried facets and faceted crusts. Evidence of the problem is clear: there has been an ongoing parade of natural and human triggered avalanches reported from all but the sunniest aspects all week. Be wary of traveling below steep, connected slopes: many of these avalanches were triggered remotely from low angle terrain and we continue to observe natural releases from wind loading. While slabs are generally soft and 1 to 2 feet thick below treeline, they will be thicker and denser in wind drifted terrain at higher elevations.
In much of the SE Mountains, this avalanche problem is mostly small in size at lower elevations and allowing for MODERATE avalanche danger at those elevations. Remember that even a small avalanche can pile deeply into a terrain trap, or push you into trees and exposed rocks.