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 surface hoar, 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 shallow below treeline, they will be thicker and denser in wind drifted terrain at higher elevations.