Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
People could trigger small slab avalanches of wind drifted snow if they venture onto exposed upper elevation slopes. It is always wise to avoid travel on steep slopes with obvious deposits of wind drifted snow.
- Suspect wind drifts or wind slabs are often smooth and rounded looking, like lenses or flying saucers.
- Wind slabs often form on the lee side of exposed ridges and in and around terrain features. Watch for and avoid drifts on gully walls, under cliff bands, along sub-ridges, in scoops, saddles, and sinks.
- Drifted snow is stiffer and more compacted than non-drifted snow, and hard drifts often produce hollow drum-like sounds when you walk on them.
- Freshly formed wind slabs can be quite sensitive and are often remotely triggered. Older, harder wind slabs can be very stubborn and may not release until you get well out on them, suddenly failing like a big mouse trap.
- Shooting cracks in drifted snow are a sure sign of instability.