Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–2.5
Some observation data continues to indicate the possibility of triggering an isolated, large avalanche, but it is becoming increasingly unlikely.
If you happen to trigger a snowpack collapse, whumpfing, or a large avalanche, you found an isolated area of instability, and it's worth pulling back from any NW-N-NE aspect avalanche terrain in the vicinity. Any isolated areas of unstable snow capable of producing a large avalanche are going to be in areas where a shallower snowpack exists, such as the northeastern, eastern, and southern portions of the forecast area.
Most people will not see signs of unstable snow today. That makes triggering one of these avalanches an unexpected event for most groups. Since one of these avalanches will probably be surprisingly large, choosing simpler terrain and exercising wide safety margins may help reduce the consequences in avalanche terrain. Non-avalanche terrain options on NW-N-NE aspect slopes or choosing alternative aspects are the best bet if you simply wish to avoid this low likelihood-high consequence problem.
Depending on the size of additional storms over the next week, our persistent weak layers of concern could become more reactive.
(12/18/2024)
Pointing at the lingering persistent weak layers of concern, Dec 12 facets and basal facets/depth hoar. All the snow above the right hand was accumulated during the last storm cycle. N aspect, 8,960', Price Peak NV
Photo: Sierra Avalanche Center