Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Triggering a 2-4' thick persistent slab avalanche is likely on many slopes. Persistent weak layers (sugary facets, surface hoar, or crusts) exist on most aspects and elevations. The recent storm formed or thickened slabs everywhere, and the weak layers are widespread. This means you could trigger a large, dangerous avalanche on just about any steep slope you encounter, even at lower elevations and in terrain sheltered from the wind.
Ben and I got a good look at the Headwaters of the Salmon River (observation). Natural avalanche activity from the last storm was muted as compared to the zones to the south. The avalanches we did see were on a variety of aspects and were more common at middle and lower elevations. Despite relatively fewer natural avalanches, the snowpack was talkative. Large booming collapses shook the snow off of trees up to 1000' away (video).
Persistent slabs are tricky. While recently wind-loaded slopes are likely more dangerous, you can't simply look for and avoid obvious wind drifts. Cracking and collapsing is a reminder that the snow you're traveling on is unstable. Plan your outing expecting to be able to 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. Skiing or riding steep, consequential terrain remains a risky roll of the dice.
(12/14/2022) This very large avalanche released on the SW-face of Savier Pk in the northern Smoky Mountains.