Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Reactive wind slabs will develop and grow larger and become more dangerous as snow accumulates, especially in the afternoon. Due to the strong winds, they may act differently from your usual deposits- you could find them in unusual areas, and at lower elevations than you might expect.
You can identify these slabs by feeling for firmer or hollow snow beneath you. Search for visual clues such as pillowy drifts, cornices, or textured surfaces. Shooting cracks is also a good indicator that the snow is unstable. They are most likely to form around rocky features, on the sides of gullies, or on leeward slopes. If you find any of these identifying characteristics, steer clear of wind-loaded slopes greater than 35 degrees.
(1/1/2022)
Cracking is a strong indicator of instability in the snow. This cracking was caused by walking past a stiff wind feature.
Photo: Irene Henninger