Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
The likelihood of triggering an avalanche has trended downwards over the last few days. Signs of instability in the deeper old snow layers are becoming increasingly isolated. The most recent signs of obvious persistent slab instability were reported on January 1. Unfortunately, the consequences of triggering an avalanche remain elevated with the potential for wide propagation and larger than expected avalanches. Mid slope avalanches and avalanches occurring on slopes with numerous tracks are also a possibility. Concern for this avalanche problem exists at all elevations on W-NW-N-NE-E aspects.
The easy way to deal with this avalanche problem is to choose to travel only on sub 30 degree angle slopes without steeper slopes above or to the side. Otherwise, moving into steeper terrain should utilize cautious, skilled, unrushed snowpack assessment. Avoid writing off any clues to instability in the deeper old snow layers regardless of isolated occurrence.
Photo: Signs of persistent slab instability on January 1 near Brockway Summit, CA.