Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
This is - again - a significant loading event for our buried weak layers from November. These layers are buried deeply in the upper reaches of the Cottonwoods and may be more prone to triggering in terrain north of BCC: along the PC ridgeline, Mill Creek, and other shallower areas. I believe the Reynolds and Freds avalanches support that theory. That said, any new snow avalanche may step down into older layers. These avalanches will be most problematic on northwest to easterly facing aspects of all elevations, but we cannot rule out the other aspects at this time. Tread carefully - these are unsurvivable avalanches. Cracking and collapsing will probably not be noted; best to follow the travel advice for HIGH - avoid all avalanche terrain.
TREND: Same