Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 4
A widespread persistent weak layer (PWL) of faceted snow is now buried under feet of recent storm snow, creating dangerous avalanche conditions.
Strong winds and heavy snowfall have overloaded this weak layer, resulting in nearly 50 avalanches over the past three days, many of which were triggered naturally or remotely. With ongoing elevated winds and more overnight snowfall, avalanches on this PWL will only grow larger.
Avoid being on, underneath, or adjacent to slopes steeper than 30° in steepness. These slides can be triggered remotely, from a distance, or even from below.
A large natural avalanche on the West Desolation Ridgeline failed within a persistent weak layer of facets, approximately 5 feet deep and 1,000 feet wide. This is the type of avalanche we could see in the backcountry today. Photo: N. Burr
If water percolates down to the persistent weak layer at lower and mid elevations, it could create a significant problem. While this is a more localized issue, as many of these areas had little to no snow before the recent storm, they could still catch riders off guard—especially those attempting to avoid the higher avalanche danger at upper elevations.