ELEVATED YOUNGER DRYAS LAKE LEVELS IN THE GREAT BASIN, WESTERN U.S.A
Deltas and beaches near the mouths of large Great Basin streams were well situated to record YD climatic change. These deposits not only were linked directly to large climate fields, their high rates of sedimentation locally produced distinctive stratigraphic packages, many of which were exposed by later downcutting. Moreover, high rates of fresh-water runoff locally supported molluscan faunas, and minimized hard-water and residence-time effects on radiocarbon ages. In the eastern Great Basin, the tributary river base levels were 10-20 m higher than historic levels about 10,900-10,300 14C yr BP. In the western Great Basin, the Humboldt and Carson River base levels were 20-30 m higher about 10,380 ± 80 14C yr BP. In the southern Great Basin, the Owens River base level at Searles Lake was 60 m higher about 10,630 ± 40 14C yr BP, suggesting that mid-YD spilling of Owens Lake may have coincided with mid-YD highstands elsewhere in the Great Basin. In the Bonneville Basin, the YD highstand pluvial hydrologic index (lake area ÷ tributary area)=0.16 (historic Great Salt Lake=0.03-0.07 and Lake Bonneville highstand=0.60). Thus, the hydrologic response of the Bonneville Basin lake to excess moisture of the YD was about 27% of the last ice age highstand and about 320% of the historic average.