Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Triggering a very large avalanche is a worrisome possibility. Some of these slides will be powerful enough to destroy a house. The primary weak layer of facets and/or surface hoar on shadier aspects and crust + facet combinations on sunnier slopes are fragile and can be found on most slopes.
The odds you trigger a Persistent Slab are decreasing, but the consequences remain severe. These avalanches can break in surprising ways. Don't expect obvious signs of instability, like cracking or collapsing before triggering a slide. You can trigger them from flat or low-angle terrain long distances away from steep slopes. The only way to manage this problem is to avoid avalanche terrain, including the base of slopes that are threatened from above. ADDITIONAL DISCUSSION:This zone picked up about a foot of snow in the last week. Look for small wind slabs at upper elevations. Loose snow avalanches (sluffs) are likely in steep terrain. These small slides may run fast and far on stout crusts and have the potential to trigger the Persistent Slab problem described above.
(1/22/2024) The debris of this slide ran into a creek, a lower and mid-elevation terrain trap that is characteristic of the Banner Summit Zone. Terrain features like these multiply the consequences of these slides.