Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Recent windblown snow has formed wind slabs 1-2 feet deep on lee slopes. Several weak layers exist in the surface snow from periods of sunshine and light snow. All of this sits above mid-January's stout crust. Winds have been strong enough to transport snow, but not as intense as we are often accustomed to on Mt Hood. Many of our usual telltale signs of wind slabs (firm and textured snow surfaces) may not be obvious. Take the time to examine the bond of recent snow to older crusts before committing to slopes steeper than 35 degrees and steer around steep start zones near ridge crests when traveling on wind loaded slopes.
Example: Wind textured snow surfaces and drifts like these serves as great clues that the wind affected the snowpack and may have formed wind slabs on nearby slopes.