Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 2
After drifting by strong winds from every direction, including from the east, human-triggered avalanches of wind-drifted snow are possible on drifted slopes facing all directions. These are most likely found at upper elevations but may also exist down lower. Some wind slabs formed on weak faceted surface snow, a persistent weak layer, and these may remain sensitive to human triggering for several days after they were formed.
- Recent drifts and wind slabs are easy to identify. They are often lense-shaped or rounded and chalky looking and may produce hollow drum-like sounds when you move around on them. Wind-drifted snow is generally stiffer than the surrounding snow.
- Wind slabs are most likely on the lee side of ridges, near cornices, and around terrain features like cliff bands and gullies.
- Softer wind slabs may be sensitive and easy to trigger, and harder slabs may wait till you get out on them and then release suddenly.
- Watch for shooting cracks, a clear sign of instability, and be aware that some wind slabs may be triggered remotely.