Английская Википедия:Horseshoe Bend (Arizona)

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Файл:Horseshoe Bend panorama.jpg

Horseshoe Bend

Horseshoe Bend is a horseshoe-shaped incised meander of the Colorado River located near the town of Page, Arizona, United States. It is also referred to as the "east rim of the Grand Canyon."

Horseshoe Bend is located Шаблон:Convert downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about Шаблон:Convert southwest of Page.

It is accessible via hiking a Шаблон:Convert round trip from a parking area just off U.S. Route 89 within southwestern Page. The land south of the Bend's parking area, trail, and overlook are on the Navajo Nation territory.

Файл:Horse Shoe Bend Hike.jpg

Horseshoe Bend is popular just before sunset, as large groups of tourists make the 1/2 mile long hike down to the overlook point. (2019)

Horseshoe Bend can be viewed from the steep cliff above.

The overlook is Шаблон:Convert above sea level, and the Colorado River is at Шаблон:Convert above sea level, making it a Шаблон:Convert drop.

Geology

Horseshoe Bend is a superb example of an entrenched meander. Six million years ago, the region around Horseshoe Bend was much closer to sea level, and the Colorado River was a meandering river with a nearly level floodplain. Between sixШаблон:SfnШаблон:Sfn and five million years ago, the region began to be uplifted. This trapped the Colorado River in its bed, and the river rapidly cut downwards to produce Horseshoe Bend as we see it today.

The cause of this uplift is still a matter of research.Шаблон:SfnШаблон:Sfn One hypothesis is that uplift was a result of delamination, where the lowest layer of the North American tectonic plate below the Colorado Plateau detached and sank into the underlying mantle. This would have allowed hotter rock from the asthenosphere, the part of the Earth's mantle that underlies its tectonic plates, to rise and lift the overlying crust.Шаблон:Sfn Another possibility is that the uplift was the result of heating at the base of the crust. This transformed the lowest crustal rock from eclogite, a relatively dense rock (3.6 g/cm³) to garnet granulite, which is significantly less dense (2.9 g/cm³). This would have produced the buoyant forces needed to uplift the region.Шаблон:Sfn

Whatever the cause of the uplift, it resulted in the erosion of up to a mile of overlying sediments from the eastern Grand Canyon.Шаблон:Sfn This exposed the Navajo Sandstone, the surface rock found throughout the Horseshoe Bend area, which also forms the entire depth of the canyon walls of the Grand Canyon at Horseshoe Bend. This sandstone is notable for its crossbedding and iron concretions.

Файл:Lake Powell and The Rincon, Utah - NASA Earth Observatory.jpg

The Rincon on Lake Powell in southern Utah. It is an incised cutoff (abandoned) meander.

It is likely that the Colorado River will eventually cut through the neck of the bend, producing a natural bridge like those found at Natural Bridges National Monument in Utah. The river will then abandon Horseshoe Bend, leaving a cutoff meander resembling The Rincon further north along the Colorado River in Utah.

Tourism

For a long time Horseshoe Bend was mostly popular with nearby residents, but the yearly visitor count sharply increased with exposure through social media. Currently the lookout is a major tourist destination with more than 2 million visitors a year. The overlook is now a fee area charging $10 (Шаблон:As of) per vehicle.

References

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