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  2. Vermilion Cliffs National Monument - Wikipedia

    en.wikipedia.org/wiki/Vermilion_Cliffs_National...

    The Vermilion Cliffs are steep eroded escarpments consisting primarily of sandstone, siltstone, limestone, and shale which rise as much as 3,000 feet (910 m) above their bases. These sedimentary rocks have been deeply eroded for millions of years, exposing hundreds of layers of richly colored rock strata.

  3. Vermilion Cliffs - Wikipedia

    en.wikipedia.org/wiki/Vermilion_Cliffs

    The Vermilion Cliffs are composed of the resistant red sandstone beds of the Lower Jurassic Moenave and Kayenta Formations. [2] They are made up of deposited silt and desert dunes, cemented by infiltrated carbonates and intensely colored by red iron oxide and other minerals, particularly bluish manganese .

  4. The Wave (Arizona) - Wikipedia

    en.wikipedia.org/wiki/The_Wave_(Arizona)

    Thin ridges created by the erosion of differentially cemented, large-scale eolian cross bedding within Navajo sandstone. The Wave is a sandstone rock formation located in Arizona, US, near its northern border with Utah. The formation is situated on the slopes of the Coyote Buttes in the Paria Canyon-Vermilion Cliffs Wilderness of the Colorado ...

  5. The Wave and Coyote Buttes: How to hike the Vermilion Cliffs ...

    www.aol.com/news/wave-coyote-buttes-hike...

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  6. Paria Canyon-Vermilion Cliffs Wilderness - Wikipedia

    en.wikipedia.org/wiki/Paria_Canyon-Vermilion...

    The Paria Canyon-Vermilion Cliffs Wilderness is a 112,500 acres (455 km 2) wilderness area located in northern Arizona and southern Utah, United States, within the arid Colorado Plateau region. The wilderness is composed of broad plateaus , tall escarpments , and deep canyons .

  7. Coyote Buttes - Wikipedia

    en.wikipedia.org/wiki/Coyote_Buttes

    Coyote Buttes is a section of the Paria Canyon-Vermilion Cliffs Wilderness managed by the Bureau of Land Management (BLM), spanning extreme south-central Utah and north-central Arizona, south of US 89 halfway between Kanab, Utah and Page, Arizona. It is divided into two areas: Coyote Buttes North and Coyote Buttes South.

  8. Geology of the Bryce Canyon area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Bryce...

    Grand Canyon (A), Chocolate Cliffs (B), Vermilion Cliffs (C), White Cliffs (D), Zion Canyon (E), Gray Cliffs (F), Pink Cliffs (G), Bryce Canyon (H) The Grand Staircase is a sequence of sedimentary rock layers, first defined in the 1870s, that stretch south for 100 miles (160 km) from Bryce Canyon National Park through Zion National Park and ...

  9. Grand Staircase - Wikipedia

    en.wikipedia.org/wiki/Grand_Staircase

    View from Utah Highway 12 of Grand Staircase–Escalante National Monument. The Grand Staircase is an immense sequence of sedimentary rock layers that stretches south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park.