Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Triggering a 2-4' thick slab avalanche is possible on steep slopes. Persistent weak layers (sugary facets, surface hoar, or crusts) exist on most aspects and elevations. The widespread nature of this weak layer is unusual. Extreme wind over the Solstice reshaped the upper snowpack, thinning (scouring) some areas and building thick hard slabs in others. You're most likely to trigger one of these slides in recently wind-affected terrain.
The slab is harder/denser near Banner Summit than in our other zones, making it less sensitive to triggering by skiers and snowmobilers. This means you are not likely to experience obvious signs of instability like snowpack cracking or collapsing. However, if you do find the "sweet spot" remember that you could trigger slides remotely—from gentler terrain above, below, and to the sides of steep slopes. These avalanches may break wider than expected or higher on the slope above you.
Unfortunately, avoiding slopes steep enough to slide is the only way to effectively manage this problem. While your odds of triggering a large avalanche are decreasing, the consequences of triggering one are not. Sticking to lower-angled, wind-sheltered slopes is a tactic to effectively reduce your risk.
ADDITIONAL DISCUSSION: Today's warm weather combined with possible afternoon sunshine may release loose snow avalanches on slopes that face the sun. These should be fairly small but may pile debris deep enough to be of concern below large slopes or channeled terrain. We may also see some rain this afternoon, and certainly this evening which will spread loose snow avalanche activity to all aspects.
(12/12/2022) In the Banner Summit zone, the weak November snow is buried beneath a 3' thick dense slab.