Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
In wind-loaded terrain, the new snow is piled deeper, and could fail more easily on Friday, so it gets the nod as the official problem. But you could consider this a "new snow problem," like our friends in Utah would say. Wind slab, storm slab, snow heating up in the sun resulting in loose or slab avalanches - they all involve the new snow. Look for textured surfaces, large drifts, fresh cornices, or actively blowing snow to help determine wind-loaded slopes. Areas such as leeward ridgelines, the base of rocks, confined chutes/gullies, and convex slopes are all classic locations where wind slabs like to form. Most reported avalanche activity over the last few days involved wind-loaded terrain. Don't make the same mistake on Friday, if you suspect a slope is wind-loaded, steer around it.
That new snow could fail in other ways in sheltered areas such as loose or storm slabs. Use your uptrack tests, hand pits, and small test slopes to look for cracking of the surface or blocks of snow failing easily. If you get concerning results, dial it back and avoid all slopes over 35 degrees. These tests work well to assess wind-affected terrain as well.
(3/13/2025)
A natural wind slab up in the rocks released on Mount Snoqualmie during the early morning hours of 3/13.
Photo: Roger Strong