Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
The slow loading of the December facet layer has produced a well-established persistent slab problem across the entire forecast area. Each major storm has produced a new round of avalanche activity, but last week's storm caused things to "go off" in this zone as many slopes finally passed their breaking point.
On Saturday, near Galena Summit, skiers remotely triggered a 1.5-2' deep avalanche from low angle terrain (photo below/right, more details). I visited the site of this avalanche yesterday and found a very similar snowpack to that observed in the rest of this zone. Yesterday, in Pole Creek, a group of riders remotely triggered an avalanche that buried the road they were riding on. This happened after the 4th rider had passed through. Keep in mind that it has now been 5 days since the last major loading event and we are continuing to see human-triggered avalanches.
Conditions remain dangerous, and it's likely you'd trigger a large avalanche on most steep slopes. The best—and often only—way to manage the persistent slab problem is by sticking to lower-angled terrain. Given the possibility of remote-triggering, you'll also want to avoid being below steep slopes.
WIND SLABS: Periods of strong to extreme winds have been the theme for the past week. Yesterday brought more of the same. Although wind slabs are becoming less reactive to the weight of a skier or rider, these slabs are adding stress to the buried weak layer of snow underneath. If you do trigger a wind slab, it could "step down", failing on layers deeper in the snowpack and becoming much larger than the initial avalanche.
(1/16/2021) Avalanche on Galena Summit that was triggered remotely from 250' away on Saturday. The avalanche broke 1.5-2' deep in middle elevation terrain.