Stock Photos of Utah

The Preacher and the Pulpit, a pair of freestanding sandstone columns in the Temple of Sinawava, are surrounded by cottonwoods with their deep green spring foliage. Zion Canyon.
Location: Zion National Park, Utah
Image ID: 12501  

Cottonwoods with their deep green spring foliage contrast with the rich red Navaho sandstone cliffs of Zion Canyon.
Location: Zion National Park, Utah
Image ID: 12509  

Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12519  

Court of the Patriarchs, named for the three Hebrew prophets Abraham, Isaac and Jacob.
Location: Court of the Patriarchs, Zion National Park, Utah
Image ID: 12805  

Court of the Patriarchs, named for the three Hebrew prophets Abraham, Isaac and Jacob.
Location: Court of the Patriarchs, Zion National Park, Utah
Image ID: 12807  

Mesa Arch spans 90 feet and stands at the edge of a mesa precipice thousands of feet above the Colorado River gorge. For a few moments at sunrise the underside of the arch glows dramatically red and orange.
Location: Island in the Sky, Canyonlands National Park, Utah
Image ID: 18085  

Soda Springs Basin in Canyonlands National Park, snow covered mesas and canyons, with the Green River far below, not far from its confluence with the Colorado River. Island in the Sky.
Location: Canyonlands National Park, Utah
Image ID: 18093  

Canyonlands National Park, winter, viewed from Grandview Point. Island in the Sky.
Location: Canyonlands National Park, Utah
Image ID: 18097  

Landscape Arch in winter. Landscape Arch has an amazing 306-foot span.
Location: Landscape Arch, Arches National Park, Utah
Image ID: 18115  

Hiker in North Window, sunset, western face. North Window is a natural sandstone arch 90 feet wide and 48 feet high.
Location: North Window, Arches National Park, Utah
Image ID: 18160  

Skyline Arch spans 90 feet.
Location: Skyline Arch, Arches National Park, Utah
Image ID: 18172  

Pine Tree Arch on the Devil's Garden Trail in Arches National Park.
Location: Pine Tree Arch, Arches National Park, Utah
Image ID: 18186  

Fins. The vertical slabs of Entrada sandstone may become natural sandstone arches.
Location: Arches National Park, Utah
Image ID: 18187  

The Organ at Courthouse Towers, narrow sandstone fins towering above the surrounding flatlands.
Location: Courthouse Towers, Arches National Park, Utah
Image ID: 18195  

Soda Springs Basin from Green River Overlook, Island in the Sky, Canyonlands National Park, Utah.
Location: Canyonlands National Park, Utah
Image ID: 27840  

Hoodoos in Goblin Valley State Park, aerial panorama. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago. Aerial panoramic photograph.
Location: Goblin Valley State Park, Utah
Image ID: 37957  

Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38017  

Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38018  

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: 38019  

Wilson Arch aerial photo, Moab, Utah. Wilson Arch has a span of 91 feet (28 m) and height of 46 feet (14 m).
Location: Wilson Arch, Moab, Utah
Image ID: 38022  

Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The San Rafael Swell is in the distance.
Location: Utah
Image ID: 38026  

Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38032  

Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance.
Location: Utah
Image ID: 38064  

Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph.
Location: Utah
Image ID: 38065  

Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38066  

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: 38067  

Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38074  

Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38170  

Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38173  

Mars Desert Research Station, set amid beautiful Mars-like "Bentonite Hills", near Hanksville, Utah.
Location: Utah
Image ID: 38179