Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
The same layer of weak snow that exists in our other zones also exists in the Banner Summit Area. The big difference here is that this snow is buried beneath a dense, 3+ foot thick slab of snow. This slab of snow is "protecting" the weak layer, making it more difficult to trigger an avalanche on it. However, if you are unlucky enough to trigger a slide it is going to be large enough to snap trees and leave piles of debris many, many feet deep. If you're anything like me, that doesn't sound like something you want to encounter.
I visited this zone yesterday to look for this problem and see how it is progressing over time. I explained what I found in this video available here. When I was out there I also observed evidence of very large deep slab avalanches that failed during the storm last week. The photo at right/below shows one of the slides that I observed.
Deep slabs behave unpredictably, often failing after many riders have already traveled on a slope. Tracks on a slope are not an indication of stability. You are most likely to trigger one of these monsters in steep, rocky terrain at upper elevations. In these areas, thin spots in the snowpack created by wind scouring bring the weak layer closer to the surface. The best—and often only—way to manage a deep persistent slab problem is by sticking to lower-angled terrain. Given the possibility of remote-triggering, you'll also want to avoid being below steep slopes that have these characteristics.
(1/18/2021) This very large avalanche occured in our Banner Summit Zone, likely during last week's storm. Based on the depth and appearance of the crown it probably failed on facets buried near the base of the snowpack.