Headed out to Ant Knolls to check out the snowpack structure on the Wasatch Back. Found a generally similar snowpack to that of the central Cottonwoods, perhaps a bit shallower, with snowpack depths between 140cm - 190cm, a large 4F to 1F slab with the bottom 35-45cm being well developed 2-4mm facets. Across the board, we found generally weakening snow on the surface or developing surface hoar. We dug in multiple areas, first true N facing at 8500' and then NW facing at 9410'. While both had pretty much identical poor snowpack structures and depths, 145-155cm deep, both got no results within the stability tests - ECTX. This is starting to further confirm the idea that we are beginning to trend in the direction of dormancy of these weak faceted grains, but currently they still very much exist. I would still be nervous about stepping into steep north-facing terrain, while the likelihood is certainly decreasing that a large 1F slab still exists on the faceted grains and the consequences are still high.