Sandstone layers that have been tilted and then eroded by runoff water can sometimes form zigzag shapes - they occur frequently in the semideserts of


Sandstone layers that have been tilted and then eroded by runoff water can sometimes form zigzag shapes - they occur frequently in the semideserts of the southwestern United States, in the area of the Colorado Plateau, where these formations are described as 'flat irons'.


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Photo credit: © BERNHARD EDMAIER/SCIENCE PHOTO LIBRARY / Alamy / Afripics
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