Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Avalanche conditions remain elevated in the backcountry. A widespread buried persistent weak layer (PWL) exists on mid and upper elevation slopes facing west through north through east. Last week’s storm winds built cohesive slabs over weak, faceted snow. Our primary concern is that a person could trigger one of these wind-drifted slabs, causing it to fail 1–3 feet deep on buried facets. Any avalanche that breaks into this layer could be large, destructive, and dangerous.
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These hard slabs are becoming stubborn, but they still require only the right trigger point. A rider or a snowmobile traveling uphill or downhill—especially across a thin or shallow spot in the slab—could cause it to fail. These types of avalanches can propagate widely and may be triggered remotely. or from below. Hard wind slabs can be tricky; sometimes, allowing a person to get well out on them before suddenly releasing.
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Watch for and avoid smooth, rounded, drum-like drifts near ridgelines, sub-ridges, rock outcrops, gully walls, and rollovers. Collapsing and shooting cracks indicate instability—but may not always be present.
This video shows an extended column test from Tuesday in the Northern Bear River Range.