Buried facets at the interface of the old snow surface prior to all of the new snow from the Christmas storm events appear to be the significant reactive weak layer and player in the majority of the avalanche acitivity. Of note, after speaking with avalanche professionals from upper BCC, and snow pit test appear to confirm this, the sensitivities observed in other locales do not appear to be as reactive in the limited areas near the Brighton Perimeter. All that said, the poor structure is similar and in place in these regions of upper BCC. ECT's and CT's have not been indicating a strong propensity for propagation at mid elevations in the upper BCC over the past two days. And regardless, the limited bridging that may be going on in this isolated area is not enough to instill strong confidence.

The sustained upper elevation winds have been active for the past 48 hours, and upper elevaiton terrain may still be suspect. Mid elevation wind slabs were observed and they were stubborn and unreactive. Saturdays forecast indicates continued "breezy" conditions, and this may keep the potential for isolated pockets of wind slabs possible on slopes on the right side of the compass. These possibilities may increase slightly overnight and into Saturday.