Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1
Below treeline and near treeline terrain that is above 8,200' on NW-N-NE-E aspects is where any lingering persistent slab instability is most likely to exist. Faceted snow that is generally found 6 inches to 2 feet below the snow surface has become wet in some areas but remains dry to moist in other areas, especially around 9,000' and above. Open areas below treeline and near treeline with good protection from NE winds is where the facets had become weakest prior to the last round of storms. These same areas are the focus of lingering concern for this avalanche problem.
Keep in mind that triggering of a persistent slab avalanche could very well occur on the mid or lower portion of the slope, rather than near the top like a wind slab avalanche.