No lack of fresh wind slabs in above tree line alpine terrain, mostly above 10,000'. These are both hard and soft. Most sit on top of the low density new snow from before the wind so they are not cracking very much or collapsing. I didn't get on any steep slopes to test them, though. Occasionally, I could find some places where the wind slabs sat on weak, shallow, faceted snow and they were much more touchy. I suspect this was the situation for the human triggered avalanches yesterday.

In the shallow snowpack areas, the added load of wind deposited snow and the expected new snow over the next several days will undoubtedly overload various layers of weak, faceted snow. It's going to be almost impossible to know where the danger areas are located because the snowpack is extremely spatially variable. In general, the areas outside of the Cottonwood Canyons are weaker and the steep, thin, rocky areas as well. Plus, there are the repeater slide paths. It's just going to be a crap shoot.