Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
A hefty, 1.5-2.5 foot thick slab lays over a delicate weak layer. In wind-loaded terrain, the slab may be twice this thick. This slab + weak layer combination exists on most slopes and has produced countless avalanches in recent days, including numerous large, remotely triggered slides. Digging into the snow you'll find a layer of snow that resembles an early-season weak layer: thick facet stacks on colder aspects, crusts with associated facets on sunnier slopes, and a good helping of surface hoar sprinkled in.
Avalanches that fail on this fragile layer will break widely and in surprising ways. These slides can be triggered from long distances away (remote triggering) and can extend back into lower angle terrain. Smaller avalanches involving snow near the surface like we are expecting today can step down to this weak snow to produce larger, more destructive slides. Today's direct sunshine and warm temperatures continue to add 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).
(1/19/2024) This photo shows several large avalanches that were remotely-triggered by riders in the Beaver Creek drainage. The furthest away slide is over 800 feet wide, and failed a half mile from where the avalanches were triggered, out of sight on the right side of the photo.