Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 3
Triggering an avalanche 2-4' deep down into our old PWL persistent weak layer of facets and crusts is becoming less likely in most terrain. The most recent reported avalanche into these facets was on Saturday December 9th in the Wilson Chutes. While snow pits continue to show poor structure; cracking and collapsing have become much less common. I suspect that in the days ahead it will become harder to trigger this layer as reports come in of rounding facets in deeper snowpack areas.
I do think you would be more likely to trigger one of these avalanches in thinner snowpack areas, such as along the Park City ridgeline, upper Mill Creek, Lambs Canyon, the Wasatch Back, or lower canyon drainages with a much shallower snowpack (read more about avalanches that involve PWL's HERE).
Cracking and collapsing may or may not accompany unstable slopes.