Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 3
Triggering an avalanche 1-3' deep down into our old PWL persistent weak layer of facets and crusts is becoming less likely. Snow pits continue to show poor structure; cracking and collapsing have become much less common and not seeing these signs does not mean a slope is stable. Extended Column Tests from recent observations show stubborn propagation in snowpits throughout the range.
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 areas with a much shallower snowpack such as lower drainages in the Cottonwood Canyons. UAC forecaster Eric Trenbeath wrote a blog about his experience with PWL in the Wasatch Mountains that's worth reading about HERE.