Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Strong winds drifted snow into avalanche-starting zones, overloading many slopes with dense snow. We advise staying clear of steep, wind-drifted slopes. Hard wind slabs are most likely to be found on the lee side of major ridges and on corniced slopes, but they were also formed by cross-loading in and around terrain features like sub-ridges, gullies, and cliff bands. Hard wind slabs sometimes allow a person to get well out on them before suddenly releasing. New, shallow, soft wind slabs of yesterday's storm snow around a foot deep could be pretty sensitive.
- Avoid rounded pillows of snow that sound or feel hollow underfoot. Wind slabs are generally much stiffer than the surrounding snow.
- Shooting cracks and collapsing or whumpfs are clear signs of instability.
- Many wind slabs formed on weak faceted surface snow, now a buried persistent weak layer, and instability could last for a while.
- Some wind slab avalanches might be triggered remotely (from a distance) or from below.