Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
You could trigger a 2-4' thick persistent slab avalanche. Buried weak layers (sugary facets or crust + facet combinations) were overloaded by recent snowfall, wind-blown snow, and rain, producing hundreds of avalanches in recent days (map). Some slopes are simply waiting for a trigger to push them over the edge.
Limited observations indicate the weak layers are not as widespread in this zone, but the safe bet is to assume they exist on any given slope until proven otherwise. Slabs will be more sensitive to triggering where recently wind-loaded. You can identify these slopes by the stiffer, denser snow that keeps your skis or sled from sinking deep into the snowpack.
Unfortunately, you can't out-smart this problem with small-scale route finding. This is the type of problem that may not offer obvious signs of instability, like snowpack cracking or collapsing. Tracks on a slope do not mean it's safe. Avalanches can be triggered by the second, third, or fourth rider. They may break over 1,000' wide and several feet thick. If caught, many of these slides will be unsurvivable. Use caution today. You could remotely trigger avalanches from gentle terrain far above, below, or to the sides of steep slopes.
Additional Discussion: Triggering a wind slab avalanche is possible in recently wind-loaded terrain. Wind slabs are more likely at upper elevation. Look for smooth pillows of windblown snow near ridgelines and mid-slope terrain features like ribs and gullies. Wind slabs or a failing cornice can serve as an effective trigger for the larger and more dangerous persistent slab problem described above.
(3/12/2023) This avalanche failed on a SE slope at 9000' in Lola Creek. Based on the aspect and the appearance of the crown, this slide likely failed on a layer of facets below a melt freeze crust.