Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Unlikely
- Tamaño
- 2–3
Triggering a persistent slab avalanche is unlikely but not impossible. Persistent weak layers (facets, facets and crusts, isolated surface hoar) exist throughout the snowpack on nearly all slopes. Know that they are 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. Because these weak layers are deeply buried, any slide that initiates on them could be large and destructive.
ADDITIONAL DISCUSSION: 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. If you are sinking into wet, sloppy snow this afternoon, find a colder slope to play on.
There's still a small chance of triggering a persistent slab avalanche, primarily in terrain like shown in the photo—very steep, rocky, and wind-affected. Johnstone Peak area.