Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
To borrow words from the Flathead Avalanche Center, “shifting winds have formed several generations of wind slabs on a variety of aspects”. While cornices and surface drifts from Monday evening's easterly winds are easy to see and avoid, the older drifts are hidden beneath newer snow. Wind drifts are widely scattered upper elevation slopes and smaller and more isolated on mid elevation slopes. They will be found on almost any aspect, cross loading across gullies, well off the ridge lines into open bowls and in unusual spots. Approach the steep slopes with caution - these hard wind drifts can not be ski cut and will break above you.
Below: recent wind effects will be easier to identify. Hardesty/Wilson photo from Big Cottonwood/Provo ridge line.