Highlights of the Geologic Evolution of the Colorado River Extensional Corridor and Its River: a Field Guide Honoring the Life and Legacy of Warren Hamilton
The Geological Society of America Field Guide 55 A river is born: Highlights of the geologic evolution of the Colorado River extensional corridor and its river: A field guide honoring the life and legacy of Warren Hamilton Keith A. Howard* U.S. Geological Survey, Geology, Minerals, Energy, and Geophysics Science Center, Menlo Park, California 94025, USA P. Kyle House* U.S. Geological Survey, Geology, Minerals, Energy, and Geophysics Science Center, Flagstaff, Arizona 86001, USA Barbara E. John* Department of Geology & Geophysics, University of Wyoming, Laramie, Wyoming 82071, USA Ryan S. Crow* U.S. Geological Survey, Geology, Minerals, Energy, and Geophysics Science Center, Flagstaff, Arizona 86001, USA Philip A. Pearthree* Arizona Geological Survey, University of Arizona, Tucson, Arizona 85701, USA ABSTRACT The Colorado River extensional corridor, which stretched by a factor of 2 in the Miocene, left a series of lowland basins and intervening bedrock ranges that, at the dawn of the Pliocene, were flooded by Colorado River water newly diverted from the Colorado Plateau through Grand Canyon. This water and subsequent sediment gave birth, through a series of overflowing lakes, to an integrated Colorado River flowing to the newly opened Gulf of California. Topock Gorge, which the river now follows between the Chemehuevi and Mohave Mountains, is a major focus of this field guide, as it very nicely exposes structural, stratigraphic, and magmatic aspects of the Miocene extensional corridor, a core complex, and detachment faults as well as a pre-Cenozoic batholith. Topock Gorge also is the inferred site of a paleodivide between early Pliocene basins of newly arrived Colorado River water.
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