Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
There are persistent weak layers buried within the upper 1-2 feet of the snowpack. Buried surface hoar and small-grained facets were responsible for a snowmobile-triggered avalanche last Saturday (02/25) (pictured to the right). In the southern portion of the advisory area (West Mountain and Council Mountain), you are likely to find these buried weak layers on multiple aspects below 8000 feet. In the northern end of our advisory area (north and east of McCall), you're most likely to encounter buried weak layers on southern aspects, where facets have formed above melt-freeze crusts.
Overall, triggering a persistent slab avalanche is becoming unlikely. The likelihood of triggering a persistent slab avalanche is higher near the West Mountain zone. Digging into the snowpack is the only way to tell if buried weak layers are lurking. Even then, buried weak layers (especially buried suface hoar) can be spotty and difficult to find. Never base a "go or no-go decision" on one snow pit. The only sure way to avoid a persistent slab avalanche is to limit exposure on slopes steeper than 30 degrees.
Additional Discussion: Snowfall accompanied by south winds are forecasted to increase today, especially in the afternoon hours. New snow and wind will be adding additional load to these buried weak layers. As the snowfall increases and the snowpack begins to endure more stress, dial back your terrain choices and give yourself space from slopes steeper than 30 degrees.
(2/25/2023)
This snowmobile-triggered avalanche was on an east aspect around 7600 ft. This avalanche failed on a layer of buried surface hoar and small-grained facets.
Photo: Public