Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 4
A widespread persistent weak layer (PWL) of faceted snow is now buried under feet of recent storm snow, creating dangerous avalanche conditions. Upper-elevation terrain is the most suspect today, but mid-elevation terrain should still be treated with extreme caution.
Strong winds and heavy snowfall have overloaded this weak layer, leading to nearly 50 avalanches over the past three days, many of which were triggered naturally or remotely. With ongoing elevated winds and additional snowfall, avalanches on this PWL will continue to grow larger.
Avoid being on, underneath, or adjacent to slopes steeper than 30°. These slides can be triggered remotely, from a distance, or even from below.
Photo of a several hundred feet long crown at the top of The Ramp just below the Cutler Headwall. Debris traveled at least 1500ft down various gullies toward the Cutler Basin. This is the type of avalanche you could expect to see on the PWL. Photo: D. Debruin
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.