Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Expect increasing size and reactivity of wind slabs as you ascend in the terrain and as the day progresses. Winds continue to redistribute recent and actively falling low-density snow onto lee slopes. Firm, punchy, or cracking snow surfaces indicates that wind slabs are present in your terrain. Slabs will run efficiently atop the late November crust. Avoid all wind-loaded slopes steeper where you find continuous snow. These areas will be far more prevalent above treeline, but extend to more specific terrain near treeline such as generally east-facing sides of canyons or ravines.