Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
Friday's storm brought 16-26" of snow (1.5-2.1" of SWE) to this zone. The rapid loading pushed the layers of weak snow now buried in the upper 2-4 feet of the snowpack past their breaking points, resulting in a widespread natural avalanche cycle. On Saturday, Ethan and I observed hundreds of avalanches that failed on persistent weak layers including the slides pictured at right/above.
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. Avalanches that fail on these layers will break very wide, wrapping around multiple aspects and connecting multiple avalanche paths. These slides can run the length of an avalanche path, impacting flat terrain long distances away from steeper slopes.
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. You can reduce (but not eliminate) your risk by sticking to gentler slopes. And don't forget to pay attention to what is above you, these avalanches can be triggered from long distances away from steeper slopes.
(3/10/2023) These very lage persistent slab avalanches failed in lower and middle elevation terrain on N-NE-E aspects above Croy Canyon west of Hailey. Old ski and skin tracks are visible on the bed surface of several of these avalanches.