description Vermilion Cliffs Escarpment Overview
The Vermilion Cliffs are a long, steep escarpment of sedimentary rock extending across northern Arizona near the Utah border. Their exposed sandstone, siltstone, and shale display red, orange, and pale bands shaped by erosion, forming part of the Colorado Plateau's Grand Staircase landscape. Much of the Arizona section lies within Vermilion Cliffs National Monument, an area known for remote terrain, geological features such as Coyote Buttes, and habitat used by reintroduced California condors.
insights Ranking position
Vermilion Cliffs Escarpment ranks #7 of 54 in the Escarpment ranking, behind Ethiopian Escarpment, ahead of Serra do Mar Escarpment.
help Vermilion Cliffs Escarpment FAQ
Where is the best-known view of the Vermilion Cliffs Escarpment?
The escarpment is visible across northern Arizona near U.S. Route 89A, particularly around Marble Canyon and the approach to Navajo Bridge. Vermilion Cliffs National Monument protects a much larger backcountry landscape north of the cliff line.
Is The Wave part of Vermilion Cliffs?
Yes, The Wave lies in Coyote Buttes North within Vermilion Cliffs National Monument near the Arizona-Utah border. Entry is tightly controlled through a permit system because the sculpted sandstone is fragile and the area has no developed trail.
Why are California condors seen near Vermilion Cliffs?
The area became a major release site for the reintroduction of California condors to the wild in northern Arizona. Visitors often watch them from Navajo Bridge, where the birds use cliffs and rising air around the Colorado River corridor.
What causes the red and orange colors in the Vermilion Cliffs?
Iron-bearing minerals in the exposed sedimentary rock produce red, orange, and purple tones as they oxidize. Differential erosion then reveals bands of sandstone, siltstone, and shale in the escarpment.
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