Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2.5
Weak layers of snow that developed during dry, cold November weather continue to produce significant collapses in the snowpack as well as avalanches. Over the past week or so, people have triggered avalanches every day in frequently traveled terrain with loud whoompfing and visible cracks reported on many slopes. Some of the avalanches have occurred after the first tracks have been laid down on a slope. The weak layers of snow causing all the problems generally exist at elevations above 8,500’ and on shaded aspects where early season snow lingered. This snow became the weak layer responsible for the current and persistent avalanche threat. You’ll see slopes that have tracks but have not avalanched…this is NOT proof of stable snow!
(12/9/2023)
Remotely triggered avalanche from below the slope in the Snake River Range. NE 8500' 18" crown thickness