Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 3
The buried persistent weak layer (PWL) has become dormant and triggering an avalanche that fails on this layer is unlikely. However, you could still trigger an avalanche in isolated areas - especially where there is a thinner snowpack such as terrain along the Park City ridgeline, Lambs Canyon, and some areas in Millcreek Canyon. If you do trigger an avalanche, it could be 2-4' deep and over a few hundred feet wide.
If you are getting into big terrain where this PWL exists, you will have to continually evaluate the snowpack looking for the dangerous structure of strong snow over weak snow (see photo below). Despite the unlikelihood of triggering an avalanche, I will continue to avoid steep slopes where this dangerous structure exists.
This photo illustrates the structure of strong snow on top of weak snow down near the ground.