Many steep slopes remain suspect and one can still trigger an avalanche on - or on approach to - recently wind drifted slopes holding older sugary faceted grains. While a slab exists now in part due to the recent winds, in general it lacks great structure and connectivity currently to break out wider than - say 100' or so. Thursday's storm may provide that.

Still, the current snow structure and avalanche type will allow you to tiptoe into steep terrain and then release well above you. This is what makes these avalanches unmanageable and why yesterday very experienced skiers and guides agreed that safe "available terrain has narrowed significantly in the last 48hours".

Guide/educator Cody Hughes's take on the snowpack below.

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Polemic on Wind

Winds drift snow with little equity in regards to distribution on both a macro and micro scale. Southwest winds (from Sunday night) often favor northwest to east facing slopes...but drifts can often be found on nearly any aspect due to terrain channelling. Beyond that, winds from this direction typically pummel areas on the south side of Little Cottonwood Canyon (Maybird, Red and White Pine, etc), upper Big Cottonwood and the south end of the Park City ridgeline. More wind=more danger.

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Sluffing in the steepest terrain is possible today in the recent low density snow. These occur independent of aspect and may be enough to either gouge down into the older weak faceted snow or potentially trigger a fresh wind drift.