Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Our region experienced a widespread avalanche cycle on November 26-27. On slopes that survived the cycle, slabs have now settled to 1 to 3 feet thick over faceted snow that formed earlier this winter. In the dry weather since, the snowpack structure is gaining strength, and the problem has become isolated and difficult to trigger. Any surprises are most likely found on wind-drifted slopes with variable thickness facing west, north, or east. Slopes with consistently deep and uniform snowpacks or slopes that naturally avalanched last week offer lower-risk options for steep terrain on those aspects. Move to smaller, less consequential terrain features when in doubt.
The last persistent slab triggered in the Northwest Mountains was this remotely triggered persistent slab on a west-facing slope above the Slate River on 11/28. This slope survived the natural cycle and had the necessary ingredients: a cohesive slab over weak, early-season snow.