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The U.S. Geological Survey is conducting multidisciplinary geologic studies of several sedimentary basins in the United States under the auspices of the U.S. Geological Survey's Evolution of Sedimentary Basins Program. This report is the Utah Geological Survey's contribution to the study of the Uinta-Piceance Basin. These cross sections incorporate published stratigraphic information and reinterpret data obtained from selected exploration boreholes to illustrate the stratigraphic relationships of rocks in an area that extends south of the Crawford Mountains, across the western projection of the Uinta Mountains and Uinta Basin, and across the San Pitch Mountains and Wasatch Plateau to the northwest side of the San Rafael Swell (figs. 1 and 2). Johnson and Johnson (1991a, 1991 b), and Franczyk (1991) published cross sections of rocks in other parts of the Uinta-Piceance Basin area. The purpose of these cross sections is to illustrate the changes in lithofacies, thickness, and nomenclature of Phanerozoic stratigraphic units from a north-south perspective. None of the stratigraphic units were palinspastically restored for the cross sections.

Stratigraphic and time-stratigraphic cross sections: A north-south transect from near the Uinta Mountain axis across the Basin and Range transition zone to the western margin of the San Rafael Swell, Utah