Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
The nature of Persistent Slab Avalanches is that they can be triggered days to weeks after the last storm. They often propagate suprizingly far accross the terrain. In some cases they can be triggered remotely, from low-angle terrain or adjacent slopes. The last notable persistent slab avalanche released on December 23rd in the Northwest Mountains. This avalanche was remotly triggered from flat terrain above the avalanche.
The most suspect areas to trigger this avalanche problem, are on previously wind-loaded slopes, and terrain with slope angles near or above 35 degrees.
In the Southeast Mountains, these slabs up to 1 foot thick in sheltered locations, and significantly deeper on drifted terrain features.
12/23 - A remotely-triggered avalanche below treeline at the head of the Slate River Valley.