Took a visit to the Elizabeth Ridge area where winds and blowing, drifting snow is the norm. This northeast facing slope becomes heavily wind loaded and it is not uncommon to see some large cornice triggered slides break to the ground.
Easily triggered shallow wind slabs along the ridge lines today with steady and gusty southwest winds. None of these broke into older snow, but in bigger more open terrain and with a snow structure that is still touchy, large deeper slides would be very possible.
A couple layers in the snow pack that stood out in this area are the old snow surface prior to the bigger storms last week and a buried faceted layer near the bottom of the pack. The upper layer would crack with a clean planer shear, but not a lot of energy and no propagation with either one.
