Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Blowing and drifting snow has formed new wind slabs on leeward slopes that face primarily NW through E, but the gusty, erratic behavior of the winds may have deposited snow on a variety of aspects. Look for fresh drifts on the leeward sides of terrain features such as sub ridges, gully walls, and rock outcroppings. Fresh drifts are recognizable by their smooth, rounded appearance, and cracking is a sign of instability. On northerly aspects, wind drifted snow has added stress to older slabs on top of a buried persistent weak layer and dangerous, human triggered avalanches 2'-3' deep are possible. Avoid steep, wind drifted slopes, especially those that face the north side of the compass.