Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
We know for sure that (at least) the Wenatchee Mountains are dangerous. Heavy slabs from solid dumps of snow the past few days are sitting over weak, sugary snow and crusts from December. Don't trust big, open slopes near and above treeline. Keep your distance from slopes 30 degrees and steeper, because this problem is unmanageable. The most dangerous slopes will be steep, open starting zones, but unsuspecting slopes at mid elevations are candidates for these deep avalanches as well. Look out for obvious signs of instability like recent deep avalanches, whumphing collapses, or shooting cracks. The next couple of days will be a good time to be patient, and stay off of steep, open slopes as the storms continue to stress these deep weak layers.
Weak snow above a crust is a tricky and historically deadly weak layer east of the crest. This structure may be anywhere from 1.5ft to 4+ft below the surface, above roughly 5,000ft. In the Wenatchee Mountains, it appears most recent activity has probably been on the 12/21 crust (which is near the ground there). In the southern half of the zone, a few potential crust layers exist. In the northern half, weak snow above a crust from early December is more concerning, as the 12/21 crust did not form there.
(1/5/2021) This chunk of slope was observed to have failed on a crust from December 21st. It was triggered by a snowcat driving by at Mission Ridge.