As described above, a layer of very small facets next to an ice crust has been producing slab avalanches. If the issue was solely the new snow, then this problem would have stabilized by now. Unfortunately this layer will continue to be a concern, but it shouldn't last nearly as long as other persistent weak layers. A process currently occurring again on the snow surface (described in this video) likely formed this layer early last week during cold temperatures and brief moment of clear weather.

Here's the good news - This layer mostly exists on slopes that should have an ice crust on the surface this morning, and those are ones you will likely avoid anyway. Northerly facing slopes seem to lack this layer and will have better snow. I don't think east facing slopes have this layer but there is some uncertainty because it has been found on east facing slopes north of Logan.

Photo below of a slide that brok on this layer near Logan near Tony Grove on Mt Magog (southeast 9600') that was 3' deep and 1500' wide.

Toby's profile from the flank of this avalanche. Similar layering has been found from Provo to Logan.

Winds have mostly been light over the last few days except at the highest elevations. They blew from the west and northwest and formed slabs of wind drifted snow over last weekend that many people triggered. Today, these many of these winds slabs should have stabilized, but winds may still be moving some snow. I would still look for and avoid these wind slabs.