Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Triggering a persistent slab avalanche is unlikely but not impossible. Deeply buried, persistent weak layers (facets, facets and crusts, isolated surface hoar) exist on nearly all slopes. Know that they are under your feet or sled. Warm and dry conditions last week finally gave these weak layers some time to rest, but they did 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. Because these weak layers are deeply buried, any slide that fails on them will be large and destructive.
ADDITIONAL DISCUSSION: Isolated wind slabs formed in "extreme" terrain in the past couple of days. Though 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.
(3/5/2021) Persistent weak layers in the Banner Summit zone are unlikely to produce avalanches - but they're still there. Here, a layer of surface hoar 3' down didn't fail during a snowpack test, but sheared when the block was pried out of the column. N, 8400'.