Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Persistent weak layers are fairly widespread across multiple aspects. The more isolated component of the avalanche problem is the distribution of slabs above those weak layers. Use caution around previously wind-loaded terrain features and higher-elevation concave bowls, where there is an increased chance of finding those slabs. Human-triggered avalanches are possible where you find this strong over weak layering. A triggered avalanche will most likely be small in size, but in very isolated areas, there could be enough mass for a large avalanche to occur.
An example of a natural avalanche observed on Monday (northeast-facing above treeline). You can trigger a similar avalanche on wind-drifted slopes facing the north half of the compass today. (12/1/2025)