Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Our snowpack is plagued by two prominent persistent weak layers:
- 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 a remotely-triggered slide in Beaver Creek (photo).
- 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 recent slide near McDonald Peak (photo to right/below). This layer is trending towards a deep persistent slab problem: difficult to trigger but terrible consequences if you do.
We are just removed from a multi-day wind event that loaded many middle and upper elevation slopes. Avoiding "prime time" avalanche terrain—slopes over about 35*—with drifts or hard snow at the surface will greatly reduce your chances of triggering a persistent slab avalanche. Keep in mind that these slides can be triggered remotely—from below, above, and to the sides of steeper terrain. Hard slabs that support the weight of skiers and sledders are notorious for producing avalanches that break wider or higher than expected.
(2/9/2021) Crown and debris from a large natural avalanche on McDonald Peak in the southern Sawtooths. This slide occurred sometime overnight on Sunday, during the ongoing wind event that loaded many slopes with stiff, dense slabs, and scoured many others. Visible are textures that indicate scouring (in the upper left) and loading (in the bottom right).