Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–2.5
Layers of weak snow buried underneath 1-2.5' 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 (photo at right/above). The slide broke over 1,000' wide and 2' deep (more details here). I triggered a similarly large slide on Sunday north of Banner Summit (video here). On Thursday, Ethan observed poor snowpack test scores on a crust + facet weak layer near McDonald Pk (photo). 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.
(4/5/2023) This avalanche was remotely triggered by two snowmobilers from a meadow 50 yds to the side of the slope. The slide broke over 1,000' wide and 2' deep. Thatcher Ck, near Copper Mtn. E and SE aspects around 8,500'.