We may see a few avalanches to the ground. These may be explosive triggered, natural, or human triggered. The heavy snowfall and sustained winds may be too much for some of our northerly terrain with a creaky snowpack; particularly areas that have previously avalanched to near the ground this year. Any fresh wind slab or new snow avalanche may step down into this older layering of weak snow.

Particularly dangerous areas would include Snake Creek, upper American Fork, upper Mill Creek and much of the Park City ridgeline.

Strong winds will continue to move snow into wind drifts that may be increasingly stubborn and less reactive as the day wears on. The wind drift may be well off the ridgelines, cross-loaded across the landscape, and may release on not the first but perhaps second or third rider across the slope. Cracking and collapsing may or may not be evident.