Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2–3
There are two persistent weak layers of concern in our snowpack:
- A thin layer of facets and sporadic surface hoar buried about 1.5-2' deep. This layer formed during a week of cold, dry weather, and was quickly loaded by the late-January snowpocalypse. It appears to be responsible for a significant portion of the recent avalanche activity in this zone. On Wednesday, Ben triggered a very large slab avalanche from a safe, low-angle ridge in Hyndman Creek (video).
- Our well-known layer of December facets buried about 3' deep. In contrast to our newer weak layer, this layer formed over a long period (3+ weeks) and was very slowly loaded. Now that it's deeply buried, it's behaving more like a deep slab problem. In other words, difficult to trigger with terrible consequences if you do.
We are in the midst of a multi-day wind event that is producing strong W to NW winds. These winds are loading many slopes at middle and upper elevations, keeping these weak layers on edge. Several large avalanches released Friday on Della Mtn above Hailey, likely as a result of fresh wind loading. Avoiding slopes over 35 degrees and/or those that have been affected by the wind will greatly reduce your chances of triggering a persistent slab avalanche.
(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.