Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Avoid recent drifts or wind slabs on steep slopes. Drifting of this week's fresh snow by strong south and west winds created wind slabs on the lee side of major ridges and in and around terrain features like sub ridges, gully walls, mid-slope roll-overs, and under cliff bands. People could trigger wind slab avalanches on steep drifted slopes at all elevations, but most likely on upper elevation slopes facing northwest through southeast.
- Even small avalanches of wind-drifted snow could run fast and far on the slick crust formed during last week's warm temperatures.
- Wind slabs are made up of stiffer or heavier snow that may be more supportable than the surrounding powder. Lense-shaped drifts often make hollow, drum-like sounds.
- Cracking is an obvious sign of wind slab instability. But, avalanches may still occur when no instability red flags are apparent.
- Soft slab and loose avalanches of new snow are possible in more sheltered terrain on slopes steeper than 30° at all elevations.