Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
A persistent weak layer of faceted snow that developed during the cold dry period in mid November exists on almost all aspects and elevation bands in the La Sal range. The buried PWL does not exist below treeline (BTL) on slopes that face SW-S-SE. Very dangerous avalanche conditions exist on any slope that harbors this buried PWL. The storm has overloaded the buried weak layer and will likely produce natural avalanches on slopes that face NW-N-E. Strong winds associated with the storm have complicated this problem. Wind drifted snow has put additional weight on these buried weak layers stressing them to their breaking point. Any avalanche triggered in a fresh wind drift has the potential to step down and trigger a more dangerous and deep avalanche failing on a buried PWL. Human triggered avalanches are very likely today, and travel in avalanche terrain is not recommended. Stick to low angle slopes with no steep terrain above you.