Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2.5
Last week's storm produced a widespread avalanche cycle on November 26-27. Many avalanches failed 2 to 4 feet deep on weak, faceted snow that formed earlier this winter. The snowpack is gradually adjusting now: stability tests are improving and signs of instability have diminished as the problem has become isolated and difficult to trigger. The most problematic slopes face west, north, and east, along with higher-elevation, southeast-facing slopes. 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 or low-angle terrain when in doubt.
A remotely triggered persistent slab on a west-facing slope above the Slate River was triggered on 11/28. This slope survived the natural cycle and had the necessary ingredients: a cohesive slab over weak, early-season snow.