Very large feathers of surface hoar rest atop a bed of loose sugary facets, now all tucked in by the new snow. This facilitated some exciting whumphs and shooting cracks as we walked up through the lower elevation terrain. The surface hoar went up to about 7800'. The facets went as high and low as we went, 6000' - 8800'. The snow sans buried surface hour didn't produce the same dramatic collapses and seemed more stubborn on our test slopes. These layers existed on every aspect we visited, NW-E. The most significant event was a 1' deep and 50' wide crack on a heavily wind loaded test slope at 7500', running on the old surface facets.

Once we got up to about 6700 feet, out of the gullies and denser trees, we were met with sporadic gusts of a pleasant breeze from the SW carrying and depositing snow. As we climbed, the winds got stronger and the signs of wind drifted snow become more prevalent. Around 7800-7900' the wind drifted snow had turned to hard slabs. These slabs did not seem connected enough to propagate into significant avalanches yet as they were sporadic and of varying harnesses and depths. On the high ridge the wind was consistently blowing very heavily, bordering unpleasant and still from the SW, and rapidly transporting snow onto the lee slopes. The south-facing slopes were deeply scoured near the ridge.