Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
A persistent slab avalanche problem continues to exist on NW-N-NE-E aspects, above 8000-8500' in mostly near and below treeline areas. This faceted snow formed near the ground and around crusts from earlier storms in October. Recent rain has strengthened this weak layer below 8000'. This next storm starting later today will add additional heavy snow on top of this weak layer and could reactivate it. Large avalanches, slope scale collapses, shooting cracks, and whumpfing sounds have all been reported over the last few days associated with this weak layer.
Recent avalanches, collapses, shooting cracks, and whumping sounds will all indicate that the weak layer is active. This avalanche problem exists in very specific terrain, with the best management technique being avoidance if traveling in these areas. Avalanches could be triggered mid-slope or even towards the bottom of slopes. Avalanches on this weak layer could be large in size with increased consequences due to the early season conditions.
(11/24/2024)
An impressive avalanche ran naturally on the upper bowl on Elephant's Back. The weak layer was sugary facets at the base of the snowpack. Carson Pass area.
Photo: David Reichel/SAC