Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
Large and dangerous avalanches stepping down into older snow on one of several buried persistent weak layers are possible, especially in areas with shallower snow and poor snow structure. Sugary weak layers exist on slopes facing every direction, not just the northern half of the compass like we saw earlier in the season. One suspect layer is found right on top of a dirty melt-freeze crust from the warm spell at the beginning of February; others consist of crust-facet sandwiches. People could trigger dangerous cornice falls and avalanches of previously drifted snow on many upper and mid-elevation slopes, but the danger is most acute on upper-elevation slopes facing northwest through southeast.
- Although most prevalent on the lee side of major ridges, stiff slabs of previously wind-drifted snow exist on all aspects in and around terrain features like sub-ridges, gullies, scoops, and cliff bands.
- 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.