We dug around 1 meter down to see how the new snow was bonding and what the old snow surface looked like. Most obvious is how dirty the recent snow came on. The dirty snow is in face snow, not the crust and was full of dirt decomposing particles.
Under the dirty snow is a crust, and underneath the crust are 1mm rounding facets. Moving down we found a generally rightside up snowpack with an impresively hard slab.
ECTN12 under the crust.
At this point the new snow seems to have bonded well with the old snow.
Overall it was a beautiful, quiet day in the Wasatch, we did not observe signs of instability in the areas that we travelled.