Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–2.5
Slabs over buried weak layers 1.5 to 3 feet thick are typically stubborn to triggers and could be reactive in a few of the shallowest areas. Obvious signs of instability are rare, and avalanches are most likely triggered from terrain features where slabs are thinner. The north half of the compass has the most fragile weak layers buried in the middle and bottom of the snowpack. Avalanches can be remotely triggered from steep or adjacent flat terrain (see several videos illustrating this) and propagate widely. The most reliable strategy for managing this problem is to choose conservative slope angles or travel on southerly aspects where the snowpack structure is more spring-like. On problematic aspects, avoid traveling in or near steep terrain where slabs are thin or variable in thickness, such as convexities, rocky areas, or wind-affected terrain.
Recent persistent slab activity from Upper Cement Creek. (3/3/2026)