Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
As is often the case in our windy range, you will wind slabs distributed widely across the terrain. You'll even find them lower in the woods following high winds on Tuesday. Most of the wind slabs in avalanche terrain will be stubborn to human triggering due the firm nature of the upper slab and a weak layer beneath that is not particularly weak (likely just 1 hardness step). False unstable tests are common in these slabs which rightly identify a planar, weak layer of softer snow or ice crust interface but fail to account for the strength of the overlying slab. Hollow sounding areas of smooth snow and energetic shooting cracks are good indicators that you’ve found a wind slab. Firm slabs typically require a thin spot for a person to trigger them but the increased load to trigger them could also come from continued loading of more wind blown snow.
Evaluate the consequences of triggering even a small slide and make your terrain choices accordingly. Long sliding falls may be possible where the wind has stripped any new snow, exposing a refrozen crust formed from a warm period Sunday morning. Carrying proper self-arrest tools will be your only ability to stop if you begin a sliding fall on even low angle slopes.