Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
The most recent activity on this layer has been at elevations above a melt-freeze crust that formed on December 26th. Thin, rocky areas above 2000m where the December 26th melt-freeze crust is thinner or non-existent continue to be areas of concern to trigger both Dec and Nov persistent weak layers.