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  2. Geology of the Grand Canyon area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Grand...

    The resulting Grand Canyon Supergroup of sedimentary units is composed of nine varied geologic formations that were laid down from 1.2 billion and 740 million years ago in this sea. [11] Good exposures of the supergroup can be seen in eastern Grand Canyon in the Inner Gorge and from Desert View, Lipan Point and Moran point. [12] [note 1]

  3. Grand Canyon - Wikipedia

    en.wikipedia.org/wiki/Grand_Canyon

    The Grand Canyon [a] is a steep-sided canyon carved by the Colorado River in Arizona, United States.The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,093 feet or 1,857 meters).

  4. History of the Grand Canyon area - Wikipedia

    en.wikipedia.org/wiki/History_of_the_Grand...

    In 1901 the Grand Canyon Railway was opened from Williams, Arizona, to the South Rim, and the development of formal tourist facilities, especially at Grand Canyon Village, increased dramatically. The Fred Harvey Company developed many facilities at the Grand Canyon, including the luxury El Tovar Hotel on the South Rim in 1905 and Phantom Ranch ...

  5. Geology of Arizona - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Arizona

    The Mesoproterozoic formations in the Grand Canyon are overlain by the 850 million year old, Neoproterozoic Chuar Group and Sixtymile Formation sedimentary rocks. The Great Unconformity is a famous gap in the stratigraphic record of the Grand Canyon of 900 million years between Proterozoic granitic rocks and Cambrian marine sediments. For the ...

  6. Horseshoe Bend (Arizona) - Wikipedia

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

    Horseshoe Bend is located 5 miles (8 km) downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles (6 km) southwest of Page. [ 1 ] [ 3 ] It is accessible via hiking a 1.5-mile (2.4 km) round trip from a parking area just off U.S. Route 89 within southwestern Page. [ 1 ]

  7. Supai Group - Wikipedia

    en.wikipedia.org/wiki/Supai_Group

    The disconformity between the Redwall Limestone and the Supai Group records a time of regional uplift, in which the Grand Canyon area was elevated by at least several hundred feet. Erosion carved channels in the Redwall Limestone that reach a maximum depth of 400 feet (120 m) in the western Grand Canyon. [10]

  8. Popular arch collapses in Glen Canyon National Recreation Area

    www.aol.com/news/popular-arch-collapses-glen...

    A frequently visited arch collapsed in Rock Creek Bay in Glen Canyon National Recreation Area in Utah, the National Park Service reported Friday in a news release.

  9. Redwall Limestone - Wikipedia

    en.wikipedia.org/wiki/Redwall_Limestone

    Within the Grand Canyon it varies from 14 to 38 m (46 to 125 ft). It normally thinnest in the eastern Grand Canyon. Because of erosion, this member wedges out 48 to 64 km (30 to 40 mi) south of the Grand Canyon. The Horseshoe Mesa Member is also absent from the Redwall Limestone in most of central Arizona. [1] [7]