Waiting for the snow to melt…
In conjunction with geologic mapping of four 7.5′ quadrangles along the South Platte River corridor in northeastern Colorado (Masters, Orchard, Weldona, and Fort Morgan), geochronology samples were collected and analyzed using optically stimulated luminescence (OSL), radiocarbon (14C), or U-series methods to provide age control for mapping units. This section of river corridor is largely covered by surficial deposits that formed from alluvial, eolian, and hillslope processes operating in concert with environmental changes from the Pleistocene to the present. The South Platte River originates high in the Colorado Rocky Mountains and recurrent glaciation of basin headwaters has affected river discharge and sediment supply far downstream, [...]
Knowledge graph centered on Data release of OSL, 14C, and U-series age data su with 11 nodes and 20 connections. Top connected: sediment transport, Accelerator mass spectrometry radiocarbon dating, Paleozoic stratigraphy, Geologic mapping, Cosmogenic ¹⁰Be surface exposure dating.
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