Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 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. Warm and dry conditions last week 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 and especially in the alpine. Because these weak layers are deeply buried on many slopes, slides failing on them could be large and destructive.
ADDITIONAL DISCUSSION: Ben found some fresh wind slabs in the Sawtooths on Monday (video). Though isolated and relatively small, these slabs could still be sensitive to your weight. You're most likely to find them in "extreme" terrain. Yesterday, I saw dozens of small, sun-induced, natural loose snow avalanches on SE-S aspects in the central and northern Sawtooths. Today's calm, clear weather could produce another round of similar activity on rocky, E-S-W facing slopes. 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'