The Leadville North 7.5' quadrangle lies at the northern end of the Upper Arkansas Valley, where the Continental Divide at Tennessee Pass creates a low drainage divide between the Colorado and Arkansas River watersheds. In the eastern half of the quadrangle, the Paleozoic sedimentary section dips generally 20–30 degrees east. At Tennessee Pass and Missouri Hill, the core of the Sawatch anticlinorium is mapped as displaying a tight hanging-wall syncline and foot-wall anticline within the basement-cored structure. High-angle, west-dipping, Neogene normal faults cut the eastern margin of the broad, Sawatch anticlinorium. Minor displacements along high-angle, east- and west-dipping Laramide reverse faults occurred in...
Tags: 10Be, 26Al,
Belden Formation,
Buckeye Peak,
Bull Lake glaciation,
Camp Hale, All tags...
Chaffee Group,
Chicago Ridge,
Colorado,
Colorado River,
Cooper Hill,
Dotsero Formation,
Eagle County,
Eagle River,
East Fork Arkansas River,
Geomorphology,
Gray porphyry group,
Hornblende Latite Porphyry,
Lake County,
Laramide,
Leadville,
Leadville Limestone,
Leadville Quadrangle,
Lincoln Porphyry,
Manitou Dolomite,
Minturn Formation,
Missouri Hill,
Mosquito Range,
Mount Zion,
No Name Gulch,
Pinedale Glaciation,
Rio Grande rift,
Sawatch Quartzite,
Sawatch Range,
Sawatch anticlinorium,
South Park,
St. Kevin Granite,
Structural Geology,
Tennessee Creek,
Tennessee Park,
Tennessee Pass,
Turquoise Lake,
USA,
USGS Science Data Catalog (SDC),
United States,
Upper Arkansas River,
Upper Arkansas Valley,
White Porphyry Group,
cosmogenic nuclide,
neotectonics,
pre-Bull Lake glaciation, Fewer tags
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