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+' 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.
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. In these areas, the weak layer is 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.
WIND SLABS: Periods of strong to extreme winds have been the theme for the past week. Yesterday brought more of the same. Although wind slabs are becoming less reactive to the weight of a skier or rider, these slabs are adding stress to the buried weak layer of snow underneath. If you do trigger a wind slab, it could "step down", failing on layers deeper in the snowpack and becoming much larger than the initial avalanche.
(1/14/2021) Avalanche that released south of Copper Mountain. This slope avalanched during the Solstice storm. E, 8700'