Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
While the likelihood of triggering an avalanche on a buried PWL is decreasing, the consequences of doing so are not.
Large and dangerous avalanches failing on one of several buried persistent weak layers remain possible, especially in areas with shallower snow and poor snow structure. People could trigger cornice falls and avalanches of previously and/or recently drifted snow that may then step down into deeper layers on many upper and mid-elevation slopes, and the danger is most acute on upper-elevation slopes facing northwest through southeast.
- Audible collapses (whumpfs) and shooting cracks are sure signs of instability, but these may not be present when avalanches occur.
- Avalanches failing on a buried persistent weak layer might be triggered remotely (from a distance) or from below steep slopes.