Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Two prominent persistent weak layers are worth tracking:
- Facets and isolated surface hoar buried 1-2' down: The late January and early February storms and recent multi-day wind event produced many natural and human-triggered avalanches on this layer. It was the likely culprit in countless avalanches in the past 2 weeks, including the large avalanche in the Croy Canyon photo to the right/below. Last week in the Hyndman Creek drainage, Ben remotely triggered a very large, likely unsurvivable avalanche that appeared to fail on this layer before stepping down to weak snow near the ground.
- December facets, now buried 3-4' down: The good news—this ugly layer has become harder to impact as the burial depth has increased. SAC forecasters and others are seeing fewer obvious signs of instability (like collapsing of the snowpack). The bad news—the first sign of instability you see may be a large, unsurvivable avalanche like the one Ben remotely triggered in the Hyndman Creek drainage last week. This layer is trending towards a deep persistent slab problem: difficult to trigger but terrible consequences if you do.
You are most likely to trigger a persistent slab in "prime time" avalanche terrain—slopes over about 35*—that has been loaded by the wind. Keep in mind that these slides can be triggered remotely—from below, above, and to the sides of steeper terrain.
(2/3/2021) This large slide likely occurred sometime Tuesday night (2/2) or Wednesday morning (2/3). It released on a 7,700' E-facing slope in Croy Canyon above Democrat Gulch.