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Monument Valley

Region of the Colorado Plateau, US

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  • 4 chapters
Monument Valley, Utah, USA
Domenico Convertini · CC BY-SA 2.0

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Through Sacredness, Western (genre) and Stratum

Monument Valley has been featured in many forms of media since the 1930s. Famed director John Ford used the location for a number of his Westerns. Film critic Keith Phipps wrote that "its five square miles [13 km2] have defined what decades of moviegoers think of when they imagine the American West".

Geography and geology

Monument Valley is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red coloration comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.

The buttes arising from the valley floor are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. Major rock formations include West and East Mitten Buttes, Merrick Butte, Hunts Mesa, Eagle Mesa, Sentinel Mesa, Brighams Tomb, Castle Rock, Stagecoach, Big Indian, Rain God Mesa, Spearhead Mesa, Mitchell Mesa, Mitchell Butte, Gray Whiskers, Elephant Butte, Camel Butte, Cly Butte, King-on-his-Throne, Rooster Rock, and Setting Hen. Another notable formation is Totem Pole, a highly eroded butte remanent. The valley also includes large stone structures, such as the "Eye of the Sun".

Between 1945 and 1967, the southern extent of the Monument Upwarp was mined for uranium, which occurs in scattered areas of the Shinarump Conglomerate; vanadium and copper are associated with uranium in some deposits.

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