Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Two buried weak layers of faceted snow in the snowpack continue to be triggered by skiers and riders—this is not speculation. The evidence is clear, check the avalanches tab for the recent examples from Monday and this past weekend.
- The upper weak layer is buried around 1–2 feet deep, formed during the cold weather at the end of January.
- The lower layer, near the ground, formed in November/December and has caused many large avalanches. This layer is most likely to be triggered in steep, thin snowpack areas, and repeater slopes—places that have previously avalanched. This layer continues to avalanche, continues to reload, and continues to be an issue.