The Vermilion Cliffs are steep eroded escarpments consisting primarily of sandstone, siltstone, limestone, and shale which rise as much as 3,000 feet
The Vermilion Cliffs are steep eroded escarpments consisting primarily of sandstone, siltstone, limestone, and shale which rise as much as 3,000 feet above their bases. These sedimentary rocks have been deeply eroded for millions of years, exposing hundreds of layers of richly colored rock strata.
Size: 14464px × 4064px
Location: USA
Photo credit: © mark higgins / Alamy / Afripics
License: Royalty Free
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