Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 3
Poor snowpack structure exists with consolidated slabs resting on buried persistent weak layers of loose, sugary, faceted snow on NW-NE-SE aspects near and above treeline. The most dangerous areas include places where wind-drifted snow has created slabs 1'-3' deep on top of these buried weak layers. These avalanches are becoming harder to trigger but once released, they will be large and destructive. Likely trigger points include shallower areas along slope margins, around sparse trees or rock outcroppings, or on repeat running slide paths.
Stability tests performed by Chris Benson on Tuesday were inconsistent on this ENE aspect near treeline location, possibly due to some shallowly-buried rocks. Both failure and propagation became more pronounced near the buried rocks and could illustrate that while hard-to-trigger, dense slabs resting on loose facets are still capable of producing a large and destructive avalanche if you hit a weak spot where the slab thins.