Paleoseismology of Utah, Volume 4: Seismotectonics of north-central Utah and southwestern Wyoming (SS-82) SH-ES2-B and the Dakota Group into

and the Dakota Group into a hydrocarbon exploration model for the Wasatch Plateau and Castle Valley areas

Hampton Sides gives us a magnificent history of the American conquest of the West

in part because they have undergone relatively little detailed geologic study as a result of their location within the U

Covering an area of 407 square miles (1054 square kilometers)

Paleoseismology of Utah, Volume 4: Seismotectonics of north-central Utah and southwestern Wyoming (SS-82) SH-ES2-B and the Dakota Group intoBy: M. W. West Geomorphic evidence of late Quaternary faulting and related tectonic deformation is present north of the Uinta Mountains in Uinta County, Wyoming and Summit County, Utah. A major zone of late Quaternary normal faulting, termed the Bear River fault zone, extends over 25 miles from southeast of Evanston, Wyoming to an apparent complex intersection with the North Flank fault of the Uinta Mountains in north central Utah. The Bear River