Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Persistent slab avalanche problems are still a lingering concern in isolated terrain for today. The surface hoar that was buried on 12/13 and caused human and natural triggered avalanches is still being found on N-NE aspects near treeline and below treeline in wind protected but open terrain. Yesterday the surface hoar that was found was mainly not reactive to snowpack tests and hand pits and appeared to have collapsed from the weight of the new snow above. There have been no reports of additional avalanches associated with this weak layer since Sunday but there still could be pockets were this layer is still reactive.
The 12/10 and 12/13 rain crust both formed early in the last 2 storm cycles as warm storms approached then quickly turned to cold snow. Developing near crust facets on both these layers could pose a persistent weak layer for now and into the future. These problems have been seen in the Carson Pass/Ebbetts Pass/Bear Valley area on NW-N-NE aspects 8000' to 9000'. In the Carson Pass area yesterday, snowpack tests were showing that both these layers were reactive. The 12/13 layer is down about 1' and the 12/10 layer is down around 2.5' from surface. In other areas this weak layer has not been seen.