Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2–3
The weak faceted snow that formed during January is being overloaded by several days of intense snowfall and rain. This weak layer is most commonly found below and near the treeline on northeast, north, and northwest aspects. It may lie buried several feet deep, especially in wind-loaded areas. Yesterday, it showed its reactivity on the west side of the forecast area with several collapses, massive shooting cracks, and natural avalanche activity. Click here to read the full observation.
The Old Ski Bowl weather station has picked up 2.5 inches of water (24 inches of snow) over the past three days. By this time tomorrow, we expect an additional two to four inches of water (20-40 inches of snow). This is far too much rapid change for the snowpack to adapt to and, as a result, we expect to see several large avalanches.
An avalanche on this layer would be several feet deep and have serious consequences. Stay off of and far away from steep slopes greater than 30°.