Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
There are two overlapping avalanche problems. (1) Old October snow became weak and faceted during dry weather in November and is now a persistent weak layer with a soft slab of December snow on top of it. See the obvious layers of faceted snow (bottom) and new snow (top) in the photo below. (2) Winds blowing from the south and southwest during the last week have loaded and put a hard slab on top of many slopes harboring the old, weak, faceted October snow.
The most likely place to get a slab avalanche are slopes that have both old October snow and wind drifted snow. Since winds have been mostly blowing from the south, I'd assume that any northerly facing slope near or above treeline has both these ingredients.
The dilemma is that terrain with the deepest snow is generally where this avalanche problem exists, so the main way to avoid avalanches is to ride low angle slope which are ones less than 30 degrees in steepness.