Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
Wind has been, and will continue to drive this problem. Since the recent storm, wind slab avalanches have failed within weak snow above the 2/7 melt-freeze crust. Some of these avalanches were remotely triggered and propagated widely during avalanche control work at Mission Ridge. Moderate-strong wind blew through the zone on Wednesday, and speeds are forecasted to increase even more on Thursday. That means you will encounter more terrain that is wind-affected and overloading these weak layers buried within. A change to denser or harder feeling snow underneath your equipment is a good indication that it has been influenced by the wind.
All steep open terrain is suspect with poor snowpack structure. Avalanches could be triggered from below or next to steep slopes. Small, steep test slopes or convex features can help gauge the reactivity of the upper snowpack. You can dig small hand pits and pull on blocks of snow to see how easily overlaying slabs break free from weak snow underneath. 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...if you can...
(2/23/2026)
On east aspects, very steep test slopes would produce stubborn small slabs that failed within weak snow over the 2/8 crust.
Photo: Katie Warren