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More model informationPortion of an inverted channel from the Cretaceous Ruby Ranch Member of the Cedar Mountain Formation exposed near Green River, UT. This portion is the westernmost part of Channel A, Segment 2 after Harris (1980) and part of Stop 3 of Williams et al. (2011). The outcrop shows classic fining upward trends characteristic of fluvial deposits.
Harris, 1980: http://web.gps.caltech.edu/~mpl/Harris1980.pdf Williams et al., 2011: https://repository.si.edu/bitstream/handle/10088/18267/201115.pdf?sequence=1&isAllowed=y
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