Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Southwesterly winds have drifted snow on to north and easterly aspects building slabs that may be sensitive to the weight of a skier or rider. Fresh drifts are recognizable by their smooth, rounded appearance, and cracking is a sign of instability. Look for them on the leeward sides of ridge crests and terrain features such as gully walls and sub ridges. In some areas, wind drifts old and new are overlying a layer of weak, sugary, faceted snow that formed during the dry period earlier this month. This condition isn't widespread, and the only way you will know for sure is to dig down and look. See more on this below.