Stuck a hand in the snow in a few places to confirm that yes, there are still basal facets with a whole bunch of water weight on top.
Noted several old D1 pockets high on the E and NE sides of Bald Mountain. There was also a very small pocket that had ripped just left of the climbing route "98 Pounds," which is at the bottom skiers left side of what I believe is called the "Living Room" if skiing (the NE slope beneath the Bald-Reids saddle). There was also a fair amount of old debris at the base of Scum Couloir. It appeared a small pocket had ripped at the base, but the rest of it appears to have funneled down from wind slab activity near the ridgeline above.
The bigger story to me, though, was collapsing. I ended up circumnavigating Bald Mountain today, and experienced literally dozens of collapses, without regard to aspect, ranging from a few feet to about 100 feet across. There were so many I stopped counting or investigating. It simply became a part of walking through the (sub 30 degree) snow. The only aspect I did NOT experience collapsing was SE, and that was simply because I didn't travel on that aspect. Certainly, the bullseye aspects had collapsing, but so did W-SW-S, to my surprise. It definitely felt like a "scary moderate" day.
Ironically, the terrain directly beneath the NE/E faces of Reids might have been some of the most stable snow I encountered. That said, I avoided the Living Room entirely, so unsure if it's simply waiting for a trigger. This is pure speculation, but I wonder if the lack of reactivity might have been due to stiff (P hard) slabs bridging over the weaker snow, plus certain areas with enough boulders sticking through to break up any chance at a contiguous weak layer.
Photo below of one of the bigger collapses, with attendant cracking.
