Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Two distinct weak layers of snow exist. The first is old October/November snow near the ground. The second is a layer of facets found 2–6 inches below the snow surface, sitting beneath a crust (see video). In different areas, the exact weak layer may differ, but the structure remains the same: strong over weak.
The snowpack has handled the modest load of 0.3-1.43 inches of SWE since the 17th, with very few avalanches running. Still, the structure persists. The remote-triggered avalanche on Murdock in wind-loaded terrain on Saturday reminds us that a quiet snowpack isn't always a stable one. While you'd have to head to specific, high, northerly, wind-loaded terrain to find these, it's important to give this problem a decent margin in your travels, as there's likely to be no warning signs—like cracking and collapsing—before it's possible to trigger a slide 1-2 feet deep. Wind drifts are especially suspect and worth avoiding.
Bo Torrey found full propagation yesterday near Empire Pass.