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Grand Canyon

The Grand Canyon is a colorful, steep-sided gorge, carved by the Colorado River, in northern Arizona. The canyon, considered to be among the major natural wonders of the world, is largely contained in the Grand Canyon National Park - one of the first national parks in the United States. President Theodore Roosevelt was a major proponent of the Grand Canyon area, visiting on numerous occasions to hunt mountain lions and enjoy the breathtaking scenery.

The canyon, created by the Colorado River cutting a channel over millions of years, is about 350 kilometers long, ranges in width from 6 to 29 kilometers and attains a depth of more than 1,600 m. The details of its development are still somewhat controversial. The most likely scenario is that a large lake overflowed the Kaibab Plateau about 5 million years ago, following the route taken by the Little Colorado River up to 70 million years ago. That accounts for the narrow lower (western) canyon and the much wider upper (eastern) canyon, as well as several other lines of evidence.

Aside from casual sightseeing from the South Rim (averaging 7000 feet/2134 m above sea level), whitewater rafting and hiking are especially popular. The floor of the valley is accessible by hiking, muleback, or by boat or raft from upriver. Commercially organized rafting trips, using 35-foot, 15 person "baloney boats" equipped with outboard engines, make the trip from Lee's Ferry to Diamond Creek in about six days while 18-foot rafts and dories powered only with oars and paddles, and take over two weeks to complete the journey. Sightseers are also carried over the canyon by helicopter.

The canyon was first seen by a European in 1540, García López de Cárdenas from Spain. Long before that however the area was inhabited by Native Americans who built settlements in the canyon walls.

Table of contents
1 Geography
2 Geology
3 Human history
4 External links

Geography

South Rim

North Rim

Temperatures on the North Rim are generally lower that the South Rim because of the greater elevation (8000 feet/2438 m above sea level). Heavy snowfall is common during the winter months. Views from the North Rim tend to give a better impression of the expanse of the canyon rather than the views down which characterise the South Rim.

Havasupai Indian Reservation The Havasupai Indian Reservation is in a large tributary canyon on the south side of the Colorado River, it is administered by the Havasupai Indian Tribe. Hualapai Indian Reservation

River

Geology

The Canyon is a deep (in places a mile deep) 277 miles long cut in the Colorado Plateau that exposes uplifted Proterozoic and Paleozoic strata. The exposed strata are gradually revealed by the gentle incline beginning at Lees Ferry and continuing to Phantom Ranch. At the point where the river crosses the Grand Wash Fault (near Lake Mead) the Canyon ends.

The Grand Canyon and the Colorado River drainage have developed in the last 40 million years, but the rocks that are exposed by the river's cutting action are over 1.7 billion years old. Deeper strata in the canyon are usually, but not always, older than higher strata.

The strata, from the bottom to top, are:

  • Early Proterozoic Schist and Granite: 1.7 billion years ago
    • Vishnu Schist
  • The Earlier Unconformity: 1.7 to 1.25 billion years ago
  • The Middle and Late Proterozoic Grand Canyon Supergroup: 1250 to 820 million years ago
    • The Uncar Group
    • Bass Limestone
    • Hotauta Conglomerate
    • Hakatai Shale
    • Shinumo Quartzite
    • Dox Sandstone
    • Cardena Lavas
  • Nakoweap Formation: 1 billion years ago
  • The Chuar Group: 950 million years ago
  • The Sixtymile Formation: 820 million years ago
  • The Great Unconformity: 820 to 570 million years ago
  • Paleozoic Sediments: 570 to 245 million years ago
  • The Cambrian Tonto Group: 570 to 505 million years ago
  • A Pre-Devonian Unconformity: 505 to 360 million years ago
  • Devonian Deposits: 408 to 360 million years ago
    • Devonian River Channels
    • Temple Butte Formation
  • The Redwall Limestone: 360 to 320 million years ago
    • Surprise Canyon Formation
  • The Supai Group: 320 to 286 million years ago
    • Watahomigi
    • Manakacha
    • Wescogame
    • Esplanade
  • The Hermit Shale: 286 to 245 million years ago
  • Coconino Sandstone
  • The Toroweap Formation
  • The Kaibab Formation
  • Mesozoic Geology: 245 to 66 million years ago
    • Shinarump Conglomerate
    • Moenkopi Formation
    • Chinle Shale
    • Chinle Formation
    • Moenave Formation
    • Kayenta Formation
    • Navajo Sandstone
    • Caramel Sandstones
    • Entrada Sandstones
    • San Rafael Group
    • Dakota Sandstone

Human history

Native American cultures

The Desert Culture

Little is known about these people who lived in western North America between 9,000 and 3,000 years ago. The earliest signs of life in the Grand Canyon, radiocarbon dated to older than 3,000 years, belong to them - tiny willow twig representations of animals, a few of which were pierced with tiny twig spears. The desert culture were hunters and gatherers and made baskets and sandals, and hunted with stone tipped spears. The first Europeans to find evidence of their activities were the 1934 Frazier, Eddy and Hatch expedition.

The Ancestral Puebloans (The Ancient Ones, or Anasazi)

  • The Basketmakers
  • The Pueblo Anasazi
  • Ancient Puebloan Occupation of the Grand Canyon
    • Nankoweap Canyon
    • The Unkar Delta
    • The Bright Angel Site
  • Ancient Pueblo peoples leave the Canyon
    • Beamer's Cabin

The Modern Hopi (see also Pueblo people)

Other Cultures

  • The Cohonina
  • The Singagua
  • The Pai (The People)
  • The Hualapai (The People of the Pine Trees)
  • The Havasupai (The People of the Place that is Green)
  • The Paiutes (The Water People)
  • The Dineh (The People)

European discovery and settlement

The Spanish Explorers

American Exploration

Settlement on the rim

External links





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