Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A weak snowpack structure continues to exist in higher elevation areas of the forecast region. Areas above 8700' on the Sierra Crest and above 8300' in the mountains East of Lake Tahoe still have weak snowpack layering with consistent unstable snowpack test results reported daily. Most, but not all, of these areas have weak faceted snow, even depth hoar, near the ground buried underneath 1 to 3 feet of snow. No avalanches have been reported on these weak layers up to this point with decreasing signs of instabilities. Additional future storms will reload and retest these weak layers. Avalanches are unlikely at lower elevations below these general elevation bands where a stronger and more consolidated snowpack exists.
Obvious signs of instability are hard to come by these days without digging into the snow and looking at the layers. To limit your exposure to this avalanche problem, you can recreate on non-avalanche terrain with no overhead hazard or pick areas and locations where this persistent slab avalanche problem does not exist.