Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2
The meager November snow in upper elevation avalanche starting zones barely covered the rocks before the weekend storm, and it is extremely weak and sugary due to its shallowness and sustained cold temperatures. Drifting snow from this weekend’s storm overloaded this weak faceted snow, and avalanches have been failing on the old sugary snow, now a persistent weak layer. Avalanches failing on a persistent weak layer could be triggered remotely, from a distance, or below. Cracking and collapsing (or whumpfs) are definite signs of instability.