Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
The likelihood of triggering slab avalanches will begin to decrease on Tuesday night as lowering freezing levels help the new snow settle. However, that may not be the case in wind-loaded terrain, steep or unsupported slopes, or where weak facets rest over a crust 1-3 ft below the surface. This poor structure has been most prominent on the east side of Mt.Hood, where persistent grains rest over the 2/7 crust. There have been avalanches breaking on this layer to our north in the West South zone and to our south in Central Oregon. While we haven’t seen any confirmed activity on this layer yet, I would keep it on your radar, especially in further east or data-sparse areas of Mt Hood.
The most likely spot you’ll trigger a large avalanche will be on wind-loaded terrain, so use visual clues like blowing snow, textured drifts, and sharp cornices to help you identify and avoid slopes of concern. Don’t ignore obvious signs of instability like shooting cracks, whumphing, or recent avalanches. Tweak small test slopes, use snowpack tests, and pay attention to red flags as you travel. As the snowpack starts settling, you may notice fewer signs of instability, so consider digging down before riding on steep open terrain.
(2/20/2026)
While the new snow is welcome, terrain traps like rocks, creeks, and terrain depressions remain abundant and can easily worsen the consequences of a triggered avalanche. Choose terrain with clean runouts without bone-breaking objects in the path.
Photo: Joe Dellaporta