Grand Canyon

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The Grand Canyon
Another view

The Grand Canyon is a famous canyon in Arizona, formed by the Colorado River. It is a UNESCO World Heritage Site,[1] and a National Park of the United States. It is also one of the Seven Natural Wonders of the World.

The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and is over a mile (1.83 km) (6000 feet) deep in places.[2] Nearly two billion years of the Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted by tectonic action.[3]

Evidence suggests the Colorado River established its course through the canyon at least 17 million years ago.[4][5][6] Since that time, the Colorado River continued to erode and form the canyon to the point we see it at today.

"Local erosion in the western Grand Canyon began about 17 million years ago, but a through-flowing Colorado River to the Pacific Ocean did not exist until about 5.4 million years ago... most of the downward cutting has been concentrated in the last 2.5 million years".[7]

Geology[change | change source]

Diagram showing the placement, age and thickness of the rock units exposed in the Grand Canyon.

The result of all the erosion is one of the most complete geologic columns on the planet. There are nearly 40 major sedimentary rock layers exposed in the Grand Canyon and in the Grand Canyon National Park area. They range in age from about 200 million to nearly 2 billion years old.

Most were laid down in warm, shallow seas, near ancient, long-gone sea shores in western North America. Both marine and terrestrial sediments are represented, including fossilized sand dunes from an ancient desert. There are at least 14 known unconformities in the geologic record found in the Grand Canyon area.

The major rock exposures in the Grand Canyon range in age from the almost 2 billion year old Vishnu Schist at the bottom of the Inner Gorge to the 230 million year old Kaibab Limestone on the rim.

Shown in the diagram, there is a gap of about one billion years between the stratum that is about 500 million years old (blue) and the lower level, which is about 1.5 billion years old at the top (green). This large unconformity indicates a period of erosion between two periods of deposition.

Many of the formations were deposited in warm shallow seas, near-shore environments (such as beaches), and swamps. The seashore repeatedly advanced and retreated over the edge of a proto-North America.

The great depth of the Grand Canyon and especially the height of its strata (most of which formed below sea level) was caused by 5,000 to 10,000 feet (1500 to 3000 m) uplift of the Colorado Plateau. This started about 65 million years ago during the Laramide period of orogeny (mountain-building). This uplift steepened the gradient of the Colorado River and its tributaries, which increased their speed and their ability to cut through rock.

Weather conditions during the ice ages also increased the amount of water in the Colorado River drainage system. The ancestral Colorado River responded by cutting its channel faster and deeper.

The base level and course of the Colorado River (or its ancestral equivalent) changed 5.3 million years ago when the Gulf of California opened and lowered the river's base level (its lowest point). This increased the rate of erosion and cut nearly all of the Grand Canyon's current depth by 1.2 million years ago. The stepped appearance of the rocks was caused by their varied resistance to the flow of water.[8]

Between three million and 100,000 years ago, volcanic activity deposited ash (tuff) and lava over the area which at times completely obstructed the river. These volcanic rocks are the youngest in the canyon.

Tourism[change | change source]

Time Visitors[9]
before WWII >100,000
1965 1.6 million
2000 4 million

Many people come from around the world to visit the Grand Canyon. People can also take trips floating on the Colorado River in boats and rafts. Some people like to hike in the Grand Canyon. The land on the north side of the Grand Canyon is called the North Rim. The land on the south side of the Grand Canyon is called the South Rim. There are trails leading from the North Rim and the South Rim to the bottom of the canyon. These trails lead to a place at the bottom of the canyon called Phantom Ranch. Phantom Ranch has a campground and cabins where hikers can spend the night. Some people also ride mules into the Grand Canyon. Most people who visit the Grand Canyon drive in cars to the South Rim and just look at the canyon from the rim and take pictures.

Related pages[change | change source]

References[change | change source]

  1. UNESCO, "Grand Canyon National Park"; retrieved 2012-4-18
  2. Kiver, E.P.; Harris, D.V. (1999). Geology of US Parklands. Wiley. p. 902.
  3. Geologic formations of the Grand Canyon National Park Service. Retrieved 2009-11-17
  4. Ranney, Wayne (2005). Carving Grand Canyon: evidence, theories, and mystery. Grand Canyon Association. ISBN 978-0-938216-82-7 .
  5. "Grand Canyon still grand but older". New York Times. 2008-03-07. http://www.nytimes.com/2008/03/07/science/07canyon.html?ref=us.
  6. Polyak, Victor; Hill, Carol; Asmerom, Yemane (2008-03-07). "Age and evolution of the Grand Canyon revealed by U-Pb dating of water table-type speleothems". Science 319 (5868): 1377–1380. doi:10.1126/science.1151248 . PMID 18323451 .
  7. Butler, Bill. "Evolution of the Colorado River and its tributaries including the origin and formation of the Grand Canyon. Geologic history of the Grand Canyon.". http://www.durangobill.com/Paleorivers_preface.html. Retrieved 2010-10-22.
  8. Leveson, David. "The hypothesis of differential erosion". http://academic.brooklyn.cuny.edu/geology/leveson/core/graphics/nyc_mins2/hyp_test_diff_erode.html. Retrieved 2010-10-22.
  9. Diercke 8. Besucherentwicklung im Grand Canyon Nationalpark.

Other websites[change | change source]

Media related to Grand Canyon at Wikimedia Commons

This article is about a World Heritage Site