Poor snowpack structure is still easily apparent. Now buried by several feet of newer snow there were no obvious signs of recent PWL activity in the surrounding area. The facets in the bottom of the snowpack have generally become rounded out at this elevation but are still weak and less dense than the layers that are presiding above it. I would be wary of this problem in thinner rockier areas and slopes that have had previous persistant slab avalanches, and any steeper slopes on the N - E sides of the compass.

Observed a ECTP 28 @ 34cm which occurred on a layer of rounded facets that were slightly weaker than the structure below. Colder temps have helped lock up overall structure.

Active wind transport was seen both to the north and south. Minimal transport was noted in my travels in the immediate area however there was significant transport along high elevation ridgelines, especially to the south along the No Name ridgeline (see picture). Easterly winds presided for most of the morning into the afternoon contributing to chilly temperatures. If these winds persists they have the potential to create slabs in unusual spots.