Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 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.
UAC forecaster Eric Trenbeath wrote a blog about his experience with PWL in the Wasatch Mountains that's worth reading about HERE.