Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Triggering a persistent slab avalanche is unlikely but not impossible. Persistent weak layers (facets, facets and crusts, isolated surface hoar) exist in the bottom and middle of the snowpack on most slopes. Know that they are likely to be under your feet or sled. Recent warm and dry conditions are giving these weak layers some time to rest, but they will not magically go away.
You're most likely to find trouble on very steep (approaching 40 degrees), rocky, wind-affected slopes. Terrain like this is most common at upper elevations and especially in the alpine. Because these weak layers are deeply buried, any slide that initiates on them will be large and destructive.
ADDITIONAL DISCUSSION: You may find isolated wind slabs in "extreme" terrain. Though relatively small, these slabs could be sensitive to your weight. Calm, clear weather today could produce some small, sun-induced loose snow avalanches in very steep, rocky terrain, most likely on E-S-W aspects. Think about the consequences of being caught in even a small slide before committing to serious, exposed terrain.
(3/3/2021) Crown of a large slab avalanche in the Sawtooth Mountains. This slide failed on a S/SE facing slope at 8,800'