Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3
"Weak snow near the ground" is the mantra of the winter. Two months ago, we buried a widespread, thick layer of facets. This layer has been responsible for the vast majority of the avalanche activity we've seen since. Unfortunately, it's shown few signs of improvement.
Recent storms have deposited thick, dense slabs at the snow surface, making this layer harder to impact. In some portions of the zone, we're headed toward a low-probability but high-consequence avalanche problem. Your odds of triggering an avalanche on this layer are relatively low, but the resulting slide would be large and destructive.
These avalanches are most likely in very steep, rocky, wind-affected terrain where more "trigger points" exist. Trigger points are locations where the overlying slab is thinner and the weight of you and-or your sled can more easily impact the weak layer.
ADDITIONAL DISCUSSION:Recent storms produced many natural and human-triggered avalanches on a layer of facets and surface hoar, including the large avalanche in the Croy Canyon photo to the right/below. Recent observations indicate that this layer has gained strength. However, I wouldn't discount it just yet, particularly where it presents as a standing stripe of surface hoar.
(2/3/2021) This large slide likely occurred sometime Tuesday night (2/2) or Wednesday morning (2/3). It released on a 7,700' E-facing slope in Croy Canyon above Democrat Gulch.