Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Steep, wind-loaded slopes are where you're most likely to trigger an avalanche on Tuesday. You may see subtly textured surfaces, larger wind features, or the slabs may be hidden beneath a smoother, non wind-affected layer. Reactive layers could be shallow, only a few inches thick, but they may have formed into drifts a foot or deeper. There's a small chance that non wind-loaded slopes could still avalanche with a human trigger, so start small before venturing out onto large slopes. Most storm instabilities are relatively shallow, so using test slopes or hand pits may work well for evaluating the bond above the crust or in the new snow layers. Expect drifts to be larger and more reactive as you gain elevation. If you see long, shooting cracks running from your feet or sled, this is an obvious clue to avoid nearby steeps. Steer around wind-loaded slopes greater than 35 degrees on Tuesday
We are still concerned about a subtle weak layer near a crust, buried about 2-4 feet deep. Infrequent avalanches have occurred on this layer, in wind-loaded terrain near and above treeline. Most avalanches failing on this layer happened Wednesday, 2/8, but an avalanche was reported late in the day Saturday in Canyon Creek, remotely triggered by a snowmobile. The large avalanche occurred on a 5400' north-facing slope, and was 2 feet deep. This layer may be more prevalent in Canyon Creek. It is very difficult to determine whether a slope has this weak layer, so even if you dig you may not find obvious clues as to whether the layer of concern is present on the slope. If you head out into this terrain, you are simply assuming a larger risk.
A small wind slab failing on a test slope. This is a good indicator for larger avalanches on bigger slopes. Wind slabs like this could fail on steep slopes with a human-trigger on Tuesday.
Photo: Irene Henninger