Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
In the Newberry zone, we have been finding a buried persistent weak layer of faceted snow on shaded, sheltered slopes. In the locations where we have more recently dug, it appears this layer is trending towards stabilizing. That being said, the poor structure of the snowpack still exists. I would expect that in isolated areas this layer will be more reactive to triggering. This PWL has been observed to be 1 to 1.5 feet beneath the snow surface, buried under the storm snow we received over the last couple of weeks. Persistant slab problems warrant conservative decision making when in pertinent terrain. I would recommend all riders avoid steep and unsupported slopes on these sheltered north aspects.