Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Two natural wind slab avalanches occurred yesterday in John F. Stevens Canyon. Observers reported active wind transport and new wind slab development in the Flathead and Swan Ranges. North and east wind speeds have tapered overnight, but slabs reactive to a rider's weight may be found in unusual locations on atypical aspects. Due to the recent strong winds, slabs may be lower on the slope than expected. Continued cold weather is slowing the strengthening of these wind-formed features.
Slabs can be identified by the snow your traveling through becoming deeper or denser. Cracks shooting out from your skis or sled indicate that you've found an unstable slab. Think about what would happen to you if the slope you are on avalanches. This sobering thought should direct you to slopes free of surface obstacles which would minimize the consequences of a slide.
(1/28/2023)
Blowing snow from northeast winds.
Photo: Dundas