Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
We continue to see failure and propagation in a weak layer close to the ground. This weak layer consists of crust and weak, sugary snow. This layer is a result of the early November snow and a prolonged spell of cold, dry weather. Stability tests and observations are showing all the classic signs of instability such as collapsing and shooting cracks. Stability tests are producing propagation with light to moderate force. In areas where the snowpack is thin this layer is particularly sensitive, such as the Purcell Range and aspects where the wind has created thinner coverage. The snowpack in the Cabinets also harbors this weak layer but it has been shown to be less sensitive. This weak layer seems to be gaining strength over time but may still be triggered easily at treeline and above.