Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 4
Avalanche conditions are dangerous in the backcountry. A widespread buried persistent weak layer exists on mid and upper-elevation slopes facing the northern half of the compass. Last week’s storm winds built cohesive slabs over weak, faceted snow, and Monday's storm further overloaded suspect slopes. Any avalanche that breaks into this layer will be large, destructive, and dangerous.
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Hard slab avalanches are becoming stubborn and difficult to trigger, but as we saw over the weekend, they require only hitting the right trigger point. A rider or a snowmobile traveling uphill, across the slope, 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 worse, 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.