Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Recent Avalanches: A slab avalanche was reported on Wilson Peak a week ago and several collapses were reported on Hale Bopp.
There are several weak layers buried 1 to 2’ deep that we are watching out for today. Most of the avalanches on these layers occurred a week ago above 2,500’. Unfortunately weak layers can be hard to assess in the field. Snow pit tests may not be reliable, and red flags such as whumphfing sounds, collapsing snow, or shooting cracks may not be present. The best way to manage this problem is by choosing slopes that have a clean runout which means there are no rocks or trees in them and if an avalanche was triggered the debris would fan out instead of piling up in a terrain trap. Practice safe traveling in consiquential terrain by exposing only one person at a time on the way up and down. Consider that small dry or wet loose avalanches may trigger one of these weak layers resulting in a larger avalanche than expected.
Wind Slabs may be problematic below ridgelines and convex rolls where they tend to form. The snow underneath you may feel firm and sound hollow or you may see shooting cracks, all signs you are traveling on a wind slab.
(4/11/2026) A fracture that propagated in this gully on Hale Bopp that did not slide.