Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Significant winds will build large wind slabs on lee aspects, further overloading our weak snowpack. Since the recent storm, wind slab avalanches are failing within faceted snow above the 2/7 melt-freeze crust. Some of these avalanches propagated widely during avalanche control work at Mission Ridge. Wind speeds are about to ramp up, drifting the soft surface snow into deeper slabs. At upper elevations, we expect especially sensitive avalanche conditions, and you should consider avoiding all steep slopes in wind-exposed terrain. Avalanches could be triggered from lower-angle terrain below or next to steep slopes.
So far, most of the activity has been localized to wind-loaded areas. However, all steep open terrain is suspect with poor snowpack structure. Long shooting cracks, collapses, or natural avalanches are key indicators of dangerous avalanche conditions. Small, steep test slopes or convex features can help gauge the reactivity of the upper snowpack. But given snowpack variability, be cautious about extrapolating your results too broadly. Instead, dial it back by seeking out low-angle terrain protected from the wind.
(2/23/2026)
A widely propagating and deep wind slab avalanche triggered by Mission Ridge Ski Patrol during control work. This slide is 3-3.5ft deep and failed on buried surface hoar.
Photo: Drew Carleton