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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Coyote Gulch is a tributary of the Escalante River, located in Garfield and Kane Counties in southern Utah, in the western United States. Over 25 miles (40 km) long[1], it exhibits many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls, narrow slot canyons, domes, arches, and natural bridges. A popular recreational destination, it is located within both the Grand Staircase-Escalante National Monument (upper sections)…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Coyote Gulch is a tributary of the Escalante River, located in Garfield and Kane Counties in southern Utah, in the western United States. Over 25 miles (40 km) long[1], it exhibits many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls, narrow slot canyons, domes, arches, and natural bridges. A popular recreational destination, it is located within both the Grand Staircase-Escalante National Monument (upper sections) and the Glen Canyon National Recreation Area (lower sections). The headwaters of Coyote Gulch have their origins along a 14 mile (22 km) segment of the Straight Cliffs, the eastern edge of the Kaiparowits Plateau. These intermittent streams merge to form larger branches, including Dry Fork, Big Hollow, the main branch of Coyote Gulch, and Hurricane Wash. The combined flow from these brancheshave carved a canyon up to 900 feet (300 m) deep into sandstone layers, before meeting the main channel of the Escalante River.