Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A weak layer of surface hoar buried 1-2 ft deep has shown fewer signs of reactivity. This problem will be most problematic in areas where the slab overlaying the weak layer is bigger and more cohesive. Persistent slab avalanches can break in surprising ways across terrain features. You up the chances for a perilous surprise if you step out blindly into steeper, more consequential terrain. You probably won't see any signs of instability on the surface before triggering an avalanche so testing for the buried weak layers can reduce your risk. Surface hoar can be identifiable as a thin gray line in the upper snowpack and with snowpit tests. You can reduce your risk by choosing slopes that are more planar without convexities and cliffs. Ultimately, the best way to manage the problem is to just avoid open slopes steeper than 30 degrees.
(1/7/2025)
Small rider-triggered wind slabs in the Superbowl that likely failed on the layer of buried surface hoar.
(6800, ENE)
Photo: Payton Schiff