Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
The heavy weight of the new snow will make it easier to trigger large and surprising avalanches. With a primed snowpack and plenty of weak snowpack structure in the zone, the only sure bet is avoidance of steep slopes. Stay out from underneath steep slopes, as you could trigger a slide from a distance. Keep an eye out for signs of instability such as recent avalanches, loud whumphing collapses, shooting cracks. The problem is a weak layer of facets in the lower half to third of the snowpack and often under one or two crusts. See Willie's video below for a great example of what we're dealing with.
Persistent slabs may be most likely where the snowpack is fairly shallow, but even in an area with a thicker snowpack in the zone such as near Washington Pass, they aren't out of the question. Some recent avalanches were suspected to have involved the December 8th surface hoar, about 2 feet below the surface. Older observations indicate that persistent slab avalanches on weak layers in the lower snowpack could be possible near valley bottoms and in isolated areas in the alpine, where the facets near the ground (mid-November) are still weak and may be close to getting overloaded.
Example widely propagating persistent slab near Harts Pass in March 2022.
Photo: Drew Lovell