The formation overlies the Lytle Formation and is overlain by the Glencairn Formation and comprises resistant, brown-weathered sandstones, and dark shales and siilstones, also described as bioturbated brownish sandstones with black and grey silty or shaley sandstone intervals. The formation was deposited in a variety of near-shore and/or marginal marine environments. The tracks occur in the upper part of an estuarine point bar sequence, overlain by brackish bay or lagoon deposits.[1]
Kurtz, W.J.; Lockley, M.G.; Engard, D.J. (2001), "Dinosaur tracks in the Plainview Formation, Dakota Group (Cretaceous, Albian) near Cañon City, Colorado: a preliminary report on another "Dinosaur Ridge"", The Mountain Geologist, 38: 155–164
Lockley, M.G (1987), "Dinosaur footprints from the Dakota Group of eastern Colorado", The Mountain Geologist, 24: 107–122
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