Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Weak layers of surface hoar and near surface facets were buried around December 8th under about 5", and then Friday the 13th-Wednesday the 18th: our last storm, laid down another 2 -3 feet of snow (2-3" of SWE) resting on weak layers. Mid-storm, there was a break that developed near surface facets, surface hoar, and graupel on the snow surface and was buried by the remaining 1.25+ or so feet. We were able to get moderate propagating results Wednesday on this mid storm weak layer and hard propagating results on the 12/8 layer.
Be cautious and don’t expose more than one person at a time to avalanche terrain...These persistent weak layers are not everywhere and were likely destroyed in many places where the wind, sun, and warm inverted temps helped beat them down. Likely areas that will hold these lurking weak layers are going to be in sun and wind sheltered areas. Forecasted warming temps may help to bond these weak layers sooner than colder weather but only time will tell.
Unlike storm instabilities, Persistent Slabs are commonly triggered remotely, from flat areas, and failures can propagate across terrain features like ridges, ribs, and gullies.
This problem poses one of the hardest for riders and sliders to dance around. Use good travel protocols on not only upper elevation, but also mid elevation protected slopes... Choose simple terrain to begin your day with representative inconsequential test slopes where if your sled or ski cut sends you on a ride it won’t be a big deal.
Slopes steep enough to slide should be approached with caution and the snowpack evaluated before you travel.
(12/18/2024)
Fresh, R1-D2 Natural Avalanche, East aspect of 8302 in the Lick Cr Drainage tough to see but likely failed on a combination of facets after recieving wind loading. We got Hard yet propigating results (ECTP 24) at this aproximate depth nearby in our test pit.
Photo: George Halcom