Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Strong to extreme southwest winds since Saturday afternoon formed drifts of varying thickness and hardness in wind-affected terrain. Some slabs will be thick and dense enough to break above you. Wind slabs are most common near and above treeline, but also exist on a few open slopes below treeline. Cracking or collapsing drifts are obvious signs of instability, though feedback will become more erratic now. Use visual clues to identify potential issues: slabs will look smooth and rounded, typically below ridgelines, in gullies, or behind rollovers. You can avoid the problem in wind-protected or wind-eroded slopes.
Several natural wind slabs ran in Redwell Basin on 3/5.