Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–2.5
Layers of weak snow buried underneath 1-2' thick slabs can produce large avalanches. The most recent triggered avalanche on these weak layers occurred on Wednesday when riders remotely triggered an impressive slide from 50 yards away. The slide broke over 1,000' wide and 2' deep (photos and more details here). I triggered a similarly large slide on Sunday north of Banner Summit (video here). Tuesday, on Mushroom Ridge, SAC staff experienced multiple large collapses and received poor snowpack test scores on slopes with a crust + facet weak layer. Most of the avalanches that we've observed on these layers have failed on crust + facet combinations.
Avalanches that fail on these weak layers will be large and destructive and will behave in surprising ways. Slides can be triggered from a distance away from steeper slopes. Several skiers or riders might traverse a slope before it avalanches—tracks on a slope are not an indication of stability. You can reduce your risk by staying off (and out from beneath) slopes steeper than about 35 degrees.
ADDITIONAL DISCUSSION: Older weak layers lay buried underneath very dense, 3-5' thick slabs. Triggering a very large avalanche involving these weak layers has become unlikely, but unlikely and impossible are very different things. The most recent triggered avalanche involving these older weak layers happened last Friday, when riders triggered a very large slide from over 500' away (photo and details here). Smaller triggered avalanches, natural wet snow avalanches, and failing cornices can all be effective triggers for these beasts. Being caught in one of these slides would likely be unsurvivable.
(3/31/2023) Crown of a very large avalanche that was remotely triggered by riders from at least 500 feet away on the ridgeline above. It broke 4-5 feet deep and 800+ feet wide. This slope faces W at 9,300' in the Frenchman's drainage near Smiley Creek. You can clearly see the two sets of persistent weak layers in our snowpack in this photo.