Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
People are likely to trigger dangerous slab avalanches of stiffer wind drifted snow failing on a sugary buried persistent weak layer if they venture onto exposed upper elevation slopes. Drifts and wind slabs may be hidden under today's fresh powder. Natural avalanches are likely as more fresh snow is drifted onto steep overloaded slopes.
- 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. Last night's strong winds created harder drifts (called hard slabs if they avalanche). Hard slabs are often stubborn, notorious for allowing people to get out on them before releasing, kind of like a mouse trap!
- Slab avalanches of wind drifted snow failing on a persistent weak layer might be triggered remotely, from a distance, or even below!
- Today you should avoid travel on or under steep slopes with deposits of wind drifted snow.
- Freshly formed wind slabs can be quite sensitive and are often remotely triggered.
- Shooting cracks in drifted snow are a sure sign of instability.