Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Friday marks the end of a very active weather week, but we're not quite out of the weeds yet. Wind slabs are likely still reactive in upper elevation terrain. They are deeper and more sensitive on north and east aspects. At middle elevations, both wind slab and storm slab avalanches are still on the table too. Clear signs of instability in both problems include long shooting cracks from your equipment, collapsing, and recent slab avalanches. You can find small, inconsequential test slopes indicative of the terrain you want to ski or ride to test for these signs, but as wind slabs trend more stubborn, the less likely you are to get clear feedback. Some better clues to look out for are a change to denser feeling snow underneath you, and cornice or drift development. Textured surfaces may be obscured by freshly fallen snow in areas closer to the Cascade Crest, but you can watch for blowing snow in these areas to signal where very small, fresh slabs are forming. Hand pits are also an excellent tool to test the bond of interstorm layers.
(1/7/2026)
A large (D2) natural avalanche involving most of the recent storm snow (1-2ft) on a very steep convex feature. This occured before daylight on 1/7. Moonlight, E, 4,300ft. (SS-N-D2-I)
Photo: Josh Hirshberg