Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
Snowfall in January built a hefty, 1.5-2.5 foot thick slab over an impressively fragile weak layer. In wind-loaded terrain, the slab may be twice this thick. This combination of slab + weak layer exists on most slopes and has produced countless avalanches in recent days, including numerous large, remotely triggered slides. Dig down and you'll find a layer of snow that resembles an early-season weak layer here: thick facet stacks on slopes that face away from the sun, crusts with associated facets on sunny slopes, and a good helping of surface hoar sprinkled in.
Avalanches that fail on this layer of snow will break widely and can be triggered from long distances away from the slope that slides (remote triggering). Smaller natural and human-triggered avalanches involving snow near the surface can step down to this weak snow, producing a much larger, more destructive avalanche. Warm temperatures and rain are adding stress to this layer, melting the upper snowpack and forcing it to pull itself downhill.
At the base of the snowpack, you'll find another layer of weak snow. While less likely, avalanches that step down to this weak layer will involve the entire snowpack and are likely to be unsurvivable (video).
(1/25/2024) This natural persistent slab avalanche released in the Swamp Ck drainage near 8800' on E and NE aspects (unknown exact release date).