Geologic Map of the Central Mineral Mountains (GIS of 1980 Map), Beaver County, Utah (MP 17-2dm) Media Type:PLOT The Late Cenozoic transition from

The Late Cenozoic transition from subduction-related to extension-related volcanism is recorded in the Soldiers Pass volcanic field in the map area

Twin Creek limestone - Arapien Shale relations in central Utah

The overlay

Experience a whirlwind tour of Utah with this wonderful book filled with exquisite

and peak-bagging routes in Wyoming's Wind River Range

Geologic Map of the Central Mineral Mountains (GIS of 1980 Map), Beaver County, Utah (MP 17-2dm) Media Type:PLOT The Late Cenozoic transition fromThe Mineral Mountains are located in Beaver and Millard Counties, southwestern Utah. The range is a horst located in the transition zone between the Basin and Range and Colorado Plateau (Stokes, 1977) geologic provinces. A multiple phase Tertiary pluton forms most of the range, with Paleozoic rocks exposed on the north and south and Precambrian metamorphic rocks on the west in the Roosevelt Hot S~rings KGRA (Known Geothermal Resource Area).