Monument Valley has been featured in many movies since the 1930s. Because of the movies, “five square miles of Monument Valley have defined what decades of moviegoers think of when they imagine the American West."
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 or
sand derived from it, deposited by the meandering rivers that carved the
valley. The valley's vivid red color comes from iron oxide exposed in the
weathered siltstone. The darker, blue-gray rocks in the valley get their color
from manganese oxide.
The
formations you see in the valley were left over after the forces of erosion
worked their magic on the sandstone. A geologic uplift caused the surface to
bulge and crack. Wind and water then eroded the land, and the cracks deepened
and widened into gullies and canyons, which eventually became the scenery you
see today.
We visited
Monument Valley on 10 June 2008. This is
a photograph taken by me on that visit.
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