Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
People could trigger dangerous cornice falls and avalanches of previously drifted snow on many upper and mid-elevation slopes, but the danger is most acute on upper elevation slopes facing northwest through southeast. Natural cornice falls and large wind slab avalanches are possible as a tremendous amount of fresh snow has drifted into avalanche starting zones recently. Wind slab avalanches could step down to a persistent weak layer capping a dirty crust from early February.
- Wind slabs are stiffer than surrounding snow, and they are smooth, rounded and chalky looking, and can sound hollow, like a drum when you move around on them. Today, wind slabs that were obvious yesterday could be hidden by a few inches of fresh snow.
- Although most prevalent on the lee side of major ridges, stiff slabs of previously wind-drifted snow exist on all aspects in and around terrain features like sub-ridges, gullies, scoops, and cliff bands.
- Cracking and whumpfs are sure signs of instability.