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    Given the current uncertainties in (1) precise local tectonic histories for each catchment basin, (2) variations in the local timing of sediment trapping and overtopping spillover from closed intermontaine basins within the north-south length of the Rocky Mountain source area, and (3) local differences in denudation rates, the rates of aggradation and the sedimentary provenance of trunk stream systems issuing from the mountain front (Chapin, 2008; Flowers et al., 2008; Eaton, 2008), the trunk streams feeding the depositional system of the Ogallala Formation all probably experienced unique histories. (1956) adopted member names of the Ogallala Formation in Kansas that were originally designated in the type area of Nebraska (Lugn, 1939).

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