Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Lingering, older wind slabs will generally be the only hazard to look out for in the morning on Friday throughout the zone. Although much more stubborn, these slabs could be deep enough to bury you should you trigger one. You can recognize where these might lurk by feeling for noticeably stiffer surfaces in wind-loaded terrain that sound hollow or drum-like.
Fresh wind slabs will form in areas closer to the Cascade Crest as the day progresses. These will be soft and small, but more sensitive. At middle elevations, they could form on slick crusts created by previous warming. Actively blowing snow will be your best clue to identifying where new slabs are forming. Textured snow surfaces, cornice development, and scoured surfaces on the side of slopes facing the wind can also clue you in to where both new and old slabs might be. Wind slabs generally form just below ridgelines and along gully walls, often referred to as cross loading.
(12/18/2025)
A small intentionally triggered wind slab from last week in the Mt. Hood zone. This exposed terrain is typical for wind slab formation.
Photo: Joe Dellaporta