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Canyon

From Wikipedia, the free encyclopedia

For the song, see CANYON.MID.
Grand Canyon, Arizona
Grand Canyon, Arizona
Noravank Monastery Complex and Canyon in Armenia.
Noravank Monastery Complex and Canyon in Armenia.

A canyon (rarely cañon) or gorge is a deep valley between cliffs often carved from the Earth by a river. Most canyons were formed by a process of long-time erosion from a plateau level. The cliffs form because harder rock strata that are resistant to erosion and weathering remain exposed on the valley walls. Canyons are much more common in arid areas than in wetter areas because weathering has a lesser effect in arid zones. Canyons' walls are often formed of resistant sandstones or granite. Submarine canyons are those which form underwater, generally at the mouths of rivers. The word canyon is Spanish in origin (cañón). The word canyon is generally used in the United States, while the word gorge is more common in Europe and Oceania, though it is also used in some parts of the United States and Canada. The rare word defile is occasionally used in England.

A famous example is the Grand Canyon in Arizona. In the southwestern United States, canyons are important archeologically because of the many cliff-dwellings built there, largely by the original natives, Ancient Pueblo Peoples.

Sometimes large rivers run through canyons as the result of gradual geologic uplift. These are called entrenched rivers, because they are unable to easily alter their course. The Colorado River and the Snake River in the northwestern United States are two examples of geological uplift.

Canyons often form in areas of limestone rock. Limestone is to a certain extent soluble, so cave systems form in the rock. When these collapse a canyon is left, for example in the Mendip Hills in Somerset and Yorkshire Dales in Yorkshire, England.

Contents

[edit] Largest canyons

The definition of "largest canyon" is rather imprecise, as a canyon can be "large" by its depth, length, or the total area of the canyon system. Also the inaccessibility of the major canyons in the Himalaya contributes to their not being regarded as candidates for the biggest canyon. The definition of "deepest canyon" is similarly imprecise, especially if one includes mountain canyons as well as canyons cut through relatively flat plateaus (which have a somewhat well-defined rim elevation).

The Yarlung Tsangpo Canyon, along the Brahmaputra in Tibet, China, is regarded by some as the deepest canyon in the world, and is even slightly longer than Grand Canyon. Hence it is regarded by many as the world's largest canyon, followed by the Kali Gandaki Gorge[1] in Nepal, Polung Tsangpo Canyon in Tibet, Cotahuasi Canyon (3,535m deep and the deepest in the Americas), and the Tekezé gorge (2000m+ deep and deepest in Africa).[2]

Slot canyons are very narrow canyons, often with smooth walls.

[edit] Other well-known canyons

Las Lajas Cathedral in southern Colombia was built in the Guaitara canyon
Las Lajas Cathedral in southern Colombia was built in the Guaitara canyon

Other lesser-known canyon systems include:

Other canyons in the Himalayas include:

The Blue Mountains west of Sydney in New South Wales, Australia contain many canyons carved into the sandstone rock.

[edit] Canyons on other planetary bodies

[edit] Trivia

Despite its name, Bryce Canyon is a giant natural amphitheater created by erosion.

[edit] See also

[edit] Notes

  1. ^ If one measures the depth of a canyon by the difference between the river height and the heights of the highest peaks on either side, the Kali Gandaki Gorge is the world's deepest. The portion of the river between the Dhaulagiri and Annapurna massifs is at an elevation of between 1300 metres and 2600 metres, 5500 to 6800 metres lower than the two peaks. See Annapurna (1:100,000 map), Nepal-Kartenwerk der Arbeitgemeinschaft für vergleichende Hochgebirgsforschung Nr. 9, Nelles Verlag, Munich, 1993. Also see Google Earth.
  2. ^ Ethiopia's Water Dilemma http://www.irn.org/pubs/wrr/issues/WRR.V21.N4.pdf]PDF (1.58 MiB)

[edit] External links

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