Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Very Likely
- Dimensione
- 3
Most slopes have persistent weak layers of faceted snow in the bottom half of the snowpack. New snow that fell in January has formed a slab on top of these weak layers. Imagine a building with a weak foundation but we keep adding additional floors on top - eventually the whole structure will collapse. New snow and wind drifted snow has added more floors to this unstable structure.
While most slopes have these weak layers, the slab on top is more variable. The most likely places to trigger a slide are recently wind loaded slopes where the slab is thicker and more cohesive. Recent strong winds have reached below treeline and affected many slopes.
Recent avalanche activity shows us that avalanches have gotten larger and will break 2-4 feet deep and possibly hundreds of feet wide.
THIS AVALANCHE PROBLEM IS TRICKY - Tracks on a slope do not mean it's safe. The way this avalanche problem works is that it may be the 2nd, 3rd, or even 10th person on a slope who triggers it.
Craig describes this set up in the video below
Photo below from an east facing slope shows that weak, rotten foundation in the snowpack near the ground. All the snow above it is what will avalanche.