Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Most of the avalanche hazard exists above 6000 ft, where snow coverage on Mt Hood starts to increase dramatically. Heavy, dense snowfall combined with strong winds will build fresh slabs you can easily trigger. Ridgelines and windward slopes may be stripped bare, but you'll likely find rapidly developing sharp cornices and growing wind slabs on the lee slopes of canyons and moraines. Active or recent transport forming dense, pillow-like slabs, or thick top-heavy drifts deserve your attention and avoidance. While hazards in the middle elevations are likely to be small (D1-1.5), keep in mind that with early season hazards very much in play, your typical escape routes may be limited.
At upper elevations, the storm will be intense with strong winds and blizzard conditions at times. Natural avalanches are possible and it may be easy to trigger one on a steep, open slope, even well below ridgelines. Be aware of and don't linger below large open slopes where an avalanche could descend from above. You may have to infer these from your map due to limited visibility. Sometimes when winds are this strong, it blows the snow right off the mountain. Other times, we get slabs forming well below start zones. Prepare for the uncertainty and avoid steep, relatively smooth lee slopes steeper than 35 degrees.
Shooting cracks in stiff wind drifted snow.
Photo: Joe Dellaporta