Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
More than 2' of snow, combined with moderate to strong winds have formed deep drifts on the leeward sides of ridge crests and terrain features, primarily in upper elevation terrain. These drifts are gaining strength with each passing day, but a triggered wind slab also has the potential to step down into a buried persistent weak layer. Wind drifts are recognizable by their smooth, rounded appearance and cracking is a sign of instability. Avoid steep slopes that have recent deposits of wind drifted snow.