The chances of triggering an avalanche breaking onto the PWL layer where we traveled are lower today than they were yesterday or the day before. There is still poor structure on most aspects and elevations. While things are settling out and we are seeing less in-your-face avalanche activity- this is a layer I don't trust. The Central Wasatch seems to have a deeper snowpack and may turn the corner more quickly (decrease in avalanche hazard) than periphery terrain such as Mill Creek, the Park City Ridgeline, or mid-Big Cottonwood Canyon.

There is a lot of surface snow available for transport and we noted flagging on the leeward side of things with continued loading of steep terrain on east-southeast aspects (photo below of wind-loaded terrain on the south ridge of Tuscarora)

We noted avalanche debris in the Seagull- that ran during the storm and most likely had wind affected snow as part of the slab. Unsure of weak layer as debris and crown were mostly covered back over.