Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
Weak layers are buried underneath dense, 1-4+ foot thick slabs of snow here. This combination can produce very large avalanches capable of destroying a house, and was responsible for yesterday's avalanche fatality in the Sawtooths. If you dig down, you'll find facet+crust combinations on slopes that face the sun and thicker stacks of weak facets on shaded slopes. These weak layers were producing large avalanches even before the weight of the big storm this weekend was added to the snowpack (photo at right/above). The slab overlying these weak layers will be even thicker in wind-loaded terrain (see Problem 2 below).
Avalanches that fail on these layers can break very wide, wrapping around multiple aspects and connecting multiple avalanche paths. These slides can run the length of the avalanche path, impacting flat terrain long distances away from steeper slopes. Avalanches may break much further above you on the slope than you expect and can be triggered from long distances away from steeper slopes. This happened yesterday when snowmobilers triggered a large avalanche near Smiley Creek while riding on the valley floor below. Tracks on a slope are not an indicator of stability—slides can be triggered after multiple riders of skiers have been up or down a slope. You aren't likely to get much or any direct feedback from the snowpack with a problem like this. The first indication of instability may be the large avalanche you trigger.
Managing persistent slab problems is difficult. If you want to completely eliminate the risk of triggering one of these beasts you'll have to avoid avalanche terrain and terrain exposed to hazard from above.
(3/12/2023) This avalanche failed on a SE slope at 9000' in Lola Creek. Based on the aspect and the appearance of the crown, this slide likely failed on a layer of facets below a melt freeze crust.