Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
Much of our snowpack is completely faceted at this point. On most west, north, and east-facing slopes, we've got anywhere from 1–4 feet of weak snow, comprised of a mess of facets and crusts to the ground.
In some spots, there’s a more cohesive slab between these weak layers, which is what we saw avalanche during last Tuesday/Wednesday’s storm. While this slab has mostly stabilized and weakened, making an avalanche unlikely, it’s still possible.
The concern extends beyond just today. Once we move out of this high-pressure period and begin to see more snow or wind loading, those faceted layers are likely to become active again, significantly increasing avalanche danger.
For now, we can enjoy soft turns and sunshine, but it’s important to stay aware of where the snow is faceting and where the surface feels damp. Areas holding cold, faceted snow will pose the greatest risk when we transition back into a period of low pressure.