Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–3
Recent storms built a thick slab of snow on top of a widespread weak layer. Warm temperatures have allowed this slab to settle and consolidate. Skiers and riders remotely triggered large to very large avalanches involving this snow from hundreds to thousands of feet away on each of the past five days (photo at right/above). Large avalanches will be easy to trigger again today. Expect to be able to trigger them from a distance away and to see them break wide, fail in unusual locations, and extend back into low angle slopes.
In sheltered terrain, expect to find slabs that are 1-2.5 feet thick. In terrain that has been affected by the wind, you'll find very dense, 2-5 foot thick slabs. Under these slabs, you'll find surface hoar and/or facets on shaded slopes and a melt-freeze crust with facets on top on sunny slopes. Large natural and human-triggered avalanches failing on this layer of weak snow have been observed on most aspects.
Further down in the snowpack, near the ground, another weak layer exists. Avalanches that step down to this layer of snow will send the entire season's snowpack rocketing downslope. We are starting to see activity on this layer, with two slides running on this layer in the Banner Summit zone this week (see Brooke's video below). This weak layer located at the base of the snowpack exists on upper elevation slopes and shaded mid-elevation slopes. Avalanches that break down into this snow are likely to be unsurvivable.
This set of avalanches failed sometime overnight on Wednesday, burying the highway near Galena Summit. They failed on E to SE facing slopes between 8,800 and 9,300'.