Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Persistent weak layers vary across the region but all are near an ice crust layer in the upper 1-2 ft of snowpack. A buried surface hoar layer above the crust was noted in Tuesdays forecast. Yesterday, in the East Cabinets we did not find surface hoar, but did observe a facet layer between crusts that fully propagated during testing. Evidence shows that both layers are beginning to heal, however; they could be triggered in the right locations. These layers will be more preserved on northerly aspects receiving less solar radiation, and will be more likely to release on exposed slopes with minimal anchor points.