Similar layering exists on west facing slopes - mainly ones not stripped by winds from the west. The main difference is that the layer of weak facets seems to be a little thinner and a little closer to the ground. In the photo below you can see what remains of several decomposing crusts layered with the facets. Those crust have been "chewed up" by the faceting process and are now soft and fragile.

I did an extended column test, and it propagated across the whole column after 10 taps from the wrist (ECTP10 - a bad test result).

At low elevation (7600 ft) north facing slopes, there is roughly a foot of snow with a layer of facets at the ground about 2 inches thick. This layer will likely be interrupted by ground roughness (aka -rocks, stumps, etc.) and not be a major issue. In isolated places with a very smooth, grassy slope underneath, it could be a problem.

LOOKING AHEAD - There will be two major weak layers in the snowpack. One is the facets near the ground. The other will be layers within the new snow. These layers may be a density change or a crystal change in the new snow. Fortunatley this weak layer will only last 24-48 hours. Unfortunatley the facets near the ground will be an issue for weeks ahead.