Overview
Cataract Canyon is a canyon of the Colorado River located within Canyonlands National Park and Glen Canyon National Recreation Area in southern Utah. It begins at Colorado's confluence with the Green River, and its downstream terminus is the confluence with the Dirty Devil River. The lower half of the canyon is submerged beneath Lake Powell when the lake is at its normal high water elevation of .
Geology
Cataract Canyon is cut by the Colorado River into the Colorado Plateau, a vast continental uplift comprising much of the American Southwest. Until approximately 80 million years ago, the Colorado Plateau was near sea level. Over millions of years, a series of inland oceans transgressed onto and regressed from the region, resulting in a series of horizontally deposited rock layers. Approximately 70 to 80 million years ago, a series of mountain-building events called the Laramide orogeny uplifted the entire region. The Colorado River subsequently cut through the rock layers, exposing them. The oldest rock layer visible in Cataract Canyon is the Paradox Formation, which was deposited approximately 320 million years ago.
History
Indigenous peoples, most likely of the Fremont culture, inhabited the Canyonlands area long before European settlers arrived. Rock art and ruins, at least 800 years old, have been found in Cataract Canyon.
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