Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Chances are, if you're in the alpine, you will encounter some wind-drifted snow. Smaller, fresher slabs will be more sensitive but not very big. There may be older, deeper slabs that are much harder to trigger, but will have much bigger consequences should you trigger one. Expect the chances of finding unstable slabs to be higher in areas closer to the Cascade Crest.
As you gain elevation and the trees become more sparse, start looking for clues of wind transport. Signals such as sharp drifts, textured snow surfaces, and riming on trees can all help you identify where the wind has transported snow. Remember that older slabs may be disguised by fresh snow. Identifying key terrain features will also help you navigate around this problem. Wind slabs often form just below ridge lines and cliffs, as well as along gully walls. Stomp around on a small and inconsequential test slope with characteristics reminiscent of what's written above to assess stability. If you get long, shooting cracks or feel collapsing, dial it back to more sheltered terrain.
(4/9/2025)
A photo from last season that shows some key features for identifying wind drifted snow.
Photo: Payton Schiff