Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
As days with small amounts of new snowfall continue to trickle in, the snowpack is getting time to slowly adjust to additional loading. However, the possibility of triggering a slide on a buried persistent weak layer will be on the table for some time to come. Uncertainty is high as to the tipping point of these layers. If you choose to enter avalanche terrain, be aware that at least one of these layers likely exists in the snowpack underneath you, particularly if recreating in terrain in the middle and upper elevations and on the southern half of the compass. Though not widespread, the layers most likely to produce large avalanches in this zone are found near the base of the snowpack and consist of well-developed facets and crust+facet sandwiches.
In a nutshell: be alert to the consequence of being caught in a large avalanche in the terrain you are recreating in.
You are more likely to trigger an avalanche on upper elevation, "prime-time" slopes steeper than about 35 degrees. Most upper-elevation slopes have received additional loading due to wind over the past few weeks. While triggering a wind slab is more likely, a wind slab avalanche could step down into these persistent weak layers resulting in a much larger avalanche.
(1/21/2023)
Drinkard and an older glide avalanche in the background; this avalanche type is uncommon for mid-winter, and currently not a primary concern. Weak snow exists across the whole of Togwotee, and the snowpack and depth should be assessed before committing to riding a slope. Even a simple check for depth is helpful.
Photo: Antonioli