Paleoseismology of Utah, Volume 4: Seismotectonics of north-central Utah and southwestern Wyoming (SS-82) SH-ES2-B in part because they have

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

By: Tim and Christine Conners

Slick Rock Member of the Entrada Sandstone

Geological Survey Open-File Report 02-172

Paleoseismology of Utah, Volume 4: Seismotectonics of north-central Utah and southwestern Wyoming (SS-82) SH-ES2-B in part because they haveBy: 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