Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
The reality is we don’t know much about what’s going on at mid and upper elevations in the Snoqualmie area. However, with all the recent snow and the very strong ridgetop winds, we suspect that thick hard wind slabs developed. As the storm clears and winds drop these deeper slabs could sit primed and waiting for a trigger. These may not be the softer wind slabs we often experience here in the Cascades. These could be hard slabs, several feet thick, and capable of growing very large and destructive. Avoid steep slopes below exposed ridges and cornices. Give these fresh wind slabs plenty of space and time to heal.
If you see large cornices looming over the slopes above you, look for a different route. Some of these features likely grew large and overhung during the storm. If they fall they could easily trigger the slopes below.
(12/28/2021)
Example: This very large avalanche was likely triggered by a cornice fall in steep wind loaded alpine terrain earlier this winter. You could see similar avalanches Satruday. NE-E aspcet, 5800'. SS-NC-R2-D2.5-U
Photo: Dallas Glass