Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
Wind slabs will continue to grow in size and become more reactive to a human's weight as new snow trickles in. While precipitation totals remain rather light, slabs could quickly become sensitive with minor warming and weak layers resting under recently formed slabs. It's not out of the question that a triggered wind slab could break more deeply or propagate more widely than expected, they fail on facets or buried surface hoar. This situation will become more likely as you move into upper elevations.
Wind slabs typically form just below ridgelines and within concave terrain features (cross-loading). Due to recent easterly winds, small slabs may exist on atypical slopes. Blowing or drifting snow will be your first easily identifiable sign that slabs are being built. Also keep an eye out for other visual and tactile clues such as textured surfaces, soft, freshly formed difts/cornices, and a change to denser feeling snow beneath your equipment.
(2/20/2026)
Mission Ridge: Wind slabs failing on buried surface hoar and entraining dry loose snow on the way down. These slabs were 4F+ hard and 8-10" at their deepest. Cracking can also be observed in near crust facets below the 02/07 crust. Mission patrollers reported sustained wind transport from the SW throughout the day.
Photo: Mission Ridge Pro Patrol