This morning winds are blowing from the west, and they've been way more than strong enough to drift the heavy powder from yesterday and overnight. Avalanches of wind drifted storm snow, 2 to 3 feet thick, are likely on drifted slopes at all elevations, but will be larger and even more likely for people to trigger on upper elevation slopes facing northwest through southeast.

The PWL problem is widely scattered across terrain, especially at mid and upper elevations, where thin layers of sugary snow or other weak snow grains exist in pockets, but on most aspects. At lower elevations in the Logan Zone layers of sugary faceted snow are more widespread and more prevalent on northerly facing slopes. There were many lower elevation areas with very weak faceted snow before last week's storm capped and moistened it with rain and heavy snow. The snow was particularly weak in protected lower elevation terrain, and poor snow structure and areas with unstable old snow can be found now on lots of lower elevation slopes.

Watch Drew's video about similar lower elevation conditions in the foothills above Salt Lake City:

Over two feet of heavy snow fell already with this storm and another foot of accumulation is possible in the Bear River Range today. As heavy snow stacks up on steep slopes it will be pretty unstable in some areas.
People are likely to trigger soft slab and loose avalanches of storm snow on slopes steeper than 30°. Natural avalanches are increasingly likely.