Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
There is a variable distribution of persistent weak layers within the snowpack at the mid and upper elevations on slopes facing northwest through east - including some upper elevation "sunny" slopes facing west and southeast - where it is possible to trigger an avalanche 2-4 feet deep. These weak layers are moving toward dormancy and are unlikely to provide any hints of instability, such as collapsing. I'm particularly suspicious of repeater slopes - slopes that have avalanched at least once this season - as the most likely to avalanche again. UAC staff Jeremy Collett and Joey Manship visited one of these repeater slopes on Wednesday in Butler Basin where Jeremy describes this thin snowpack structure: