Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
On specific ‘solar’ slopes, particularly those facing east and southeast, there is a persistent weak layer (PWL) of facets just above a crust buried by storms beginning February 14. As the warm weather and clear skies persist, the likelihood of triggering an avalanche on this layer will continue to decrease, and the facets will begin to heal. However, as demonstrated by this week's avalanche activity, including the massive avalanche on Mill Hiller on Thursday, we have not reached that point yet. I'm addressing this issue by avoiding these slopes and opting for northerly-facing slopes where the snow quality is superior.
Mark discusses the avalanche problem primarily isolated to the East and southeast-facing aspects.
While we are considering shrinking this avalanche problem, as it appears to be primarily isolated to southeast through east-facing aspects, there is still a chance of encountering this layering and issue on western-facing slopes.