Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Snowfall and wind over the past two weeks have created thick slabs at the upper elevations. The recently formed slabs are sitting on weak layers of snow that can be found at different depths in the snowpack. Avalanches involving these weak layers could break 2-5 feet deep, or even deeper in some locations. Steep, rocky, and wind loaded terrain on the north half of the compass is most suspect. While the sensitivity of these layers is decreasing, natural and rider triggered avalanches occurred two days ago. These events indicate that the snowpack is still adjusting to the most recent load.
Approach steep terrain in the upper elevations with suspicion. Extra caution is advised in exposed, wind affected terrain that is punctuated by rocks and cliffs. Obvious signs of instability such as collapsing may not be present. As a result, it is important to make your own stability assessment of a particular slope before committing to steep terrain. If you are unsure about a stability assessment, then defaulting to lower angle terrain is always a good call.
(2/17/2024)
This large avalanche was triggered by the second rider on a slope up Sheep Creek in the Snake River Range at 9,500 feet on an E aspect.