Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–2.5
Dense 2-3' thick slabs overlie weak layers, including sugary facets, surface hoar, and crust + facet combinations on many NW-N-NE-E aspects.
Persistent slab problems can be tricky to deal with. Don't count on obvious signs of instability like snowpack cracking or collapsing to indicate an unstable slope. Your first sign of instability may be the avalanche you trigger. Persistent slabs may be triggered remotely—from above, below, and to the sides of steep slopes.
Simply avoiding avalanche terrain where these slabs + weak layers exist is the best way to stack the odds in your favor.
Additional Discussion: Whether a weak layer exists or not, the combination of recent snowfall and moderate winds formed slabs that may remain sensitive to your weight. Watch for dunes, waves, and textured surfaces created by wind. Feel for stiff slabs overlying weaker or softer snow. These often form near exposed ridgelines. These smaller wind slabs, once moving, are an effective trigger for the larger Persistent Slab avalanches described above.