Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Prominent weak layers are buried in the upper 1-3 feet of the snowpack. Dig down and you'll find facets, surface hoar, and crust+facet combinations, depending on your aspect and elevation. Last week, during an intense storm, these layers produced a widespread natural avalanche cycle (you can view recent avalanches here). Many slides broke hundreds of feet wide. The largest slides spanned 1,500-2,000' feet of terrain (photo at right/above). These layers became less reactive and harder to impact as the slab above them stiffened, but the ongoing storm is working to wake them back up.
Avalanches that fail on these layers of weak snow will break widely and will be able to wrap around terrain features. This produces large, unpredictable avalanches with deep piles of debris that you do not want to be in. You can trigger these slides from below or near steep slopes. Completely avoiding this problem includes avoiding terrain threatened from above.
Large, 1,500-foot-wide slab avalanche that failed naturally in the Seeley Lake zone during last week's storm. Similar avalanches are possible today.
Photo: Ben VandenBos