Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–1.5
Near the Cascade Crest, small wind slabs will develop throughout the day with periods of convective snow showers. As you gain elevation and begin to find new, dry snow, start to put this problem on your radar. Wind slabs often form just below ridgelines or within concave terrain features (cross-loading). Blowing snow will be the first obvious clue of slab development. Uneven, textured surfaces and a change to denser feeling snow are other visual and tactile observations to use. Be cognizant of your terrain selection. Although small, an avalanche could easily sweep you off your feet and carry you into hazards below.
Conditions on the far northern end of the zone may be tracking more closely with the East North zone. If you encounter more than a few inches of new or recent snow in these areas at middle or upper elevations, expect larger, more widespread slab development. Fresh cornices may be larger and can serve as an identifiable clue to where the wind has recently blown snow. Consider reading the East North forecast before heading out to get a sense of how conditions could be different.
Conditions to the eastern side of the zone, primarily the Wenatchees, are generally safe. It is unlikely you will encounter enough new snow for wind slabs to exist.
(1/5/2026)
Wind slabs should be small like this in most of the zone on Wednesday. Shooting cracks clearly indicate instability.
Photo: Payton Schiff