Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A persistent weak layer - or PWL - of faceted snow exists on northerly-facing slopes at the mid and upper-level elevations where it is possible to trigger an avalanche up to 2 feet deep and over 100 feet wide. Avalanche activity and field work this week inform us that the slopes that are most prone to slide are recently wind-loaded and have a slab of stronger snow on top of the buried PWL. If you choose to venture onto steep, northerly-facing slopes, you'll have to dig down and look for this structure of strong (firmer/denser) snow over weak (softer/loose) snow, as shown in this photo where the gray stripe is the weakest snow. In my field work yesterday, I got full propagation with extended column tests where this structure exists, indicating that although avalanches are becoming less likely, they are still possible.