Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Use caution on leeward sides of ridges and terrain features. Look and feel in the snow for clues such as stiffer, deeper drifts, or sculpted surfaces. Steer around convex roll-overs and slopes 35 degrees and steeper where you see evidence of drifting.
Light snow accumulations and increasing wind will form thin slabs on older wind drifts, formed on the 15th. In most places, older slabs will be difficult to trigger. You may be able to trigger them on shaded, northerly aspects above treeline where weak snow lies under the older slabs.
(3/15/2022) An example of a wind slab avalanche from Washington Pass. Photo: Josh Hirshberg