Deva Temple

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Deva Temple
Deva Temple from Bright Angel.jpg
North aspect at sunset
Highest point
Elevation 7,353 ft (2,241 m) [1]
Prominence 693 ft (211 m) [1]
Parent peak Brahma Temple (7,551 ft) [1]
Isolation 1.56 mi (2.51 km) [1]
Coordinates 36°09′08″N112°01′54″W / 36.1521473°N 112.0318004°W / 36.1521473; -112.0318004 Coordinates: 36°09′08″N112°01′54″W / 36.1521473°N 112.0318004°W / 36.1521473; -112.0318004 [2]
Geography
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Deva Temple
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Deva Temple
Location Grand Canyon National Park
Coconino County, Arizona, US
Parent range Kaibab Plateau
Colorado Plateau
Topo map USGS Bright Angel Point
Geology
Type of rock Coconino Sandstone
Climbing
First ascent July 17, 1959 Harvey Butchart [3]

Deva Temple is a 7,353-foot-elevation (2,241-meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, USA. [2] It is situated three miles south of the North Rim's Bright Angel Point, and towers 3,700 feet (1,100 meters) above Bright Angel Canyon. Its nearest higher neighbor is Brahma Temple, 1.5 mile to the south. Other neighbors include Zoroaster Temple 2.5 miles to the south-southwest, Manu Temple three miles to the west-northwest, and Buddha Temple, 3.5 miles to the west. Deva Temple was named by Henry Gannett, a geographer for Clarence Dutton, in following Dutton's practice of naming features in the Grand Canyon after mythological deities, in this case, Deva. [2] [4] This geographical feature's name was officially adopted in 1906 by the U.S. Board on Geographic Names. [2] According to the Köppen climate classification system, Deva Temple is located in a Cold semi-arid climate zone. [5]

Contents

Geology

The summit of Deva Temple is composed of cream-colored, cliff-forming, Permian Coconino Sandstone with a small, remnant Kaibab Limestone caprock. [6] The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes. Below the Coconino Sandstone is slope-forming, Permian Hermit Formation, which in turn overlays the Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek level. [7] Precipitation runoff from Deva Temple drains south into the Colorado River via Bright Angel Creek on its west side, and Clear Creek on the east side.

See also

Related Research Articles

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<span class="mw-page-title-main">Pollux Temple</span> Landform in the Grand Canyon, Arizona

Pollux Temple is a 6,251-foot-elevation (1,905-meter) summit in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated ten miles northwest of Grand Canyon Village, and less than one mile northeast of Jicarilla Point. Castor Temple is one mile northwest, and Diana Temple is one mile southeast. Topographic relief is significant as Pollux Temple rises nearly 4,000 feet above the Colorado River in less than two miles. Pollux Temple is named for Pollux, the divine son of Zeus according to Greek mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. According to the Köppen climate classification system, Pollux Temple is located in a Cold semi-arid climate zone.

<span class="mw-page-title-main">Diana Temple (Grand Canyon)</span> Landform in the Grand Canyon, Arizona

Diana Temple is a 6,683-foot-elevation (2,037-meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated nine miles northwest of Grand Canyon Village, and immediately northeast of Mescalero Point. Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south. Topographic relief is significant as Diana Temple rises nearly 4,300 feet above the Colorado River in less than two miles. Diana Temple is named for Diana, the goddess of the hunt and the moon according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. The U.S. Geological Survey applied the name, and this geographical feature's name was officially adopted in 1908 by the U.S. Board on Geographic Names. In the early 1900s this mesa was sometimes called "No Mans Land". According to the Köppen climate classification system, Diana Temple is located in a Cold semi-arid climate zone.

<span class="mw-page-title-main">Thor Temple</span> Landform in the Grand Canyon, Arizona

Thor Temple is a 6,741-foot (2,055 m)-elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated 2.5 miles (4.0 km) west-northwest of Cape Royal on the canyon's North Rim, 3.5 miles (5.6 km) east of Brahma Temple, and 2 miles (3.2 km) north-northwest of Wotans Throne. It rises 4,300 feet (1,300 m) above the Colorado River in 5 miles (8.0 km). According to the Köppen climate classification system, Thor Temple is located in a cold semi-arid climate zone.

<span class="mw-page-title-main">Butchart Butte</span> Landform in the Grand Canyon, Arizona

Butchart Butte is a 7,602-foot (2,317 m)-elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated on the North Rim, midway between Gunther Castle and Siegfried Pyre, and between the Chuar and Kwagunt Valleys. Topographic relief is significant as it rises 4,900 feet (1,500 m) above the Colorado River in five miles.

<span class="mw-page-title-main">Manu Temple</span> Landform in the Grand Canyon, Arizona

Manu Temple is a 7,184-foot-elevation (2,190-meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated one mile south of the North Rim's Widforss Point, 1.5 miles (2.4 km) northeast of parent Buddha Temple, and three miles southwest of the North Rim's Bright Angel Point. Topographic relief is significant as it rises nearly 3,600 feet in two miles above Bright Angel Canyon to the east, and 2,200 feet in less than one mile above Haunted Canyon to the immediate west. Its neighbors include Brahma Temple and Deva Temple to the east on the opposite side of Bright Angel Canyon. From the South Rim of the canyon it may be difficult to discern Manu Temple from the walls of the Kaibab Plateau one mile behind it, but when the lighting and atmosphere are favorable, this butte of great proportions can be seen clearly defined.

<span class="mw-page-title-main">Vesta Temple</span> Landform in the Grand Canyon, Arizona

Vesta Temple is a 6,299-foot-elevation (1,920-meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north. Topographic relief is significant as Vesta Temple rises 3,900 feet above the Colorado River in 2.5 miles. Vesta Temple is named for Vesta, the goddess of the hearth, home, and family according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. This geographical feature's name was officially adopted in 1908 by the U.S. Board on Geographic Names. According to the Köppen climate classification system, Vesta Temple is located in a Cold semi-arid climate zone.

References

  1. 1 2 3 4 "Deva Temple – 7,353' AZ". Lists of John. Retrieved December 25, 2020.
  2. 1 2 3 4 "Deva Temple". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2020-12-25.
  3. "Harvey Butchart's Grand Canyon Hiking Logs". cholla.mmto.org. Retrieved 2021-01-11.
  4. Randy Moore and Kara Felicia Witt, The Grand Canyon: An Encyclopedia of Geography, History, and Culture, 2018, ABC-CLIO Publisher, p. 151.
  5. Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN   1027-5606.
  6. N.H. Darton, Story of the Grand Canyon of Arizona, 1917, p. 32.
  7. William Kenneth Hamblin, Anatomy of the Grand Canyon: Panoramas of the Canyon's Geology, 2008, Grand Canyon Association Publisher, ISBN   9781934656013.