Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Recent snowfall has formed a soft, 6-10" thick slab atop extremely weak, faceted snow that formed during the 3+ week dry spell since mid-November. Even this small load produced several small avalanches during and right after the most recent storm. While our weak layer is "something special", we still haven't added enough slab to produce widespread instability. In our northern zones where more recent snow accumulated, the snowpack is even closer to the brink. The last storm produced avalanches large enough to bury people in the Western Smokys, Sawtooths, and Banner Summit area.
Yesterday's wind was visibly transporting snow along higher ridgelines and in alpine terrain. This wind is helping to add the piece of the puzzle that's mostly missing on sheltered slopes—a thicker and denser slab on the facet layer. A small natural avalanche in wind-exposed terrain was observed yesterday in Baker Creek, and skiers in Owl Creek were able to release a small slide with a ski cut.
You can greatly decrease your chances of releasing a slide by avoiding slopes with evidence of recent wind effect—especially in the Soldiers Mountains that have received more recent snowfall and wind. Triggering an avalanche on wind-sheltered slopes is unlikely, but use extra caution on steep slopes and convexities approaching 40 degrees.
(12/17/2020) Small avalanche that ran on the faceted old snow surface in the Soldier Mountains.