Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
Additional snowfall and strong winds will continue to stress the buried persistent weak layer that has been the culprit in multiple avalanches and the two recent avalanche fatalities in the Central Wasatch (Porter Fork and Davenport Hill). Photo below (Manship) of cracking in the snowpack on an east facing slope in Dry Fork. These cracks as well as collapsing and whumpfing are signs that the buried facets are still reactive. If this slope had been any steeper this would have been an avalanche.