Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
There are two persistent weak layers of concern in the Seeley zone.
The first is a layer of buried surface hoar that can be found in both the southern Missions and southern Swans at elevations above 6000. It can be found 8" to 12 " below the surface. Slides were easily triggered on this layer on Saturday, and several were triggered yesterday in the Lake Dinah area, according to an observation received after the initial publication of the forecast this morning. In the Missions, this layer can be found on all aspects, although southern aspects may be less touchy. In the southern Swans, it is somewhat patchy. Skiers and riders are likely to trigger slides on this layer in the right terrain. Likelihood can be reduced by avoiding convex rolls over 35º and unsupported slopes.
The second layer is deeply buried facets that may still exist on shaded upper elevation terrain in the southern Swans. The recent warm temperatures are certainly helping basal facets bond. However, in shallow north-facing terrain, weak sugary facets can still be found below a cohesive slab. It is unlikely to trigger this layer, but it could happen with just the right shallow trigger spot. Sledders high marking a slope may be able to trench down and trigger this layer. Avoid shallow areas in upper elevation north aspects, such as around wind swept ridges.
(1/14/2023)
D1.5 Avalanche that slid on buried surface hoar near Marshall Lake
Photo: Caleb Kesterke