Factory Butte at sunrise. An exceptional example of solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 37018
Factory Butte at sunrise. An exceptional example of solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 37019
Factory Butte at sunrise. An exceptional example of solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 37020
Factory Butte. An exceptional example of a solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 37872
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38020
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38021
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38030
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 38047
Molly's Castle, aerial view, Goblin Valley State Park.
Location: Goblin Valley State Park, Utah
Image ID: 38049
Panorama dimensions: 3346 x 8974
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 38053
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 38056
Aerial photo of the San Rafael Reef at dawn. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39786
Panorama dimensions: 4384 x 8521