Geological situation of Buza II site location

The Buza II site is located on confluence of Buza and Enisey rivers valley. Now part of the site destroyed by Krasnoyarsk reservoir. Site location is circumscribed by snap-fault. It is located on laid down bedrock. The site is situated on diluvial sedimentary cover middle part, breached by narrows. This diluvial sedimentary cover has conical terraced structure. The sedimentary cover is built of sandy loam and has small sheet structure and loess sandy loam. The artifacts is deposited on the lower part of most recent sandy loam of diluvial sedimentary cover. This sediment is deposited above diluvial sandy loam with materials of landwastes resedimentation. The materials of landwastes resedimentation considered cameo-shells of cryophilic terraneous mollusks. It allows us to identify this sediment as norilsk stage of sartan. So sediments with artifacts can be identified by Lower Holocene.