Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
The last significant, reported avalanche in this zone occurred 20 days ago when ski patrollers at Bald Mountain intentionally triggered an avalanche during mitigation work before opening the ski area. The slide failed on a wind-loaded slope that sees little ski traffic and harbored weak, sugary, faceted snow in the lower part of the snowpack. Ben recently visited the Pioneer Mtns and found a thin, weak, generally stable snowpack (video here). Most slopes were lacking the slab part of the avalanche equation (slab+weak layer+steep slope+trigger=avalanche).
The snowpack scenario from the Baldy avalanche earlier this month—hard, wind-drifted snow overlying weak, faceted snow—is where you're most likely to find unstable conditions today. These slabs often form downwind of prominent terrain features and can sound "drummy" or feel hollow beneath your skis or sled. While triggering a slab avalanche is unlikely, I'd still pay attention in very steep, recently wind-loaded terrain, especially at elevations over about 9000'.
ADDITIONAL DISCUSSIONOn Monday near Galena Summit, a skier intentionally triggered a small, recently formed wind slab. Although less snow fell in this area last weekend, you may find similar drifts in the highest reaches of this zone. Watch for signs of recent wind-loading such as dune-like drifts and ripples in the snow surface.