Deva Temple is a 7,353-foot-elevation (2,241 meter) summit located in the

Grand Canyon The Grand Canyon (, yuf-x-yav, Wi:kaʼi:la, , Southern Paiute language: Paxa’uipi, ) is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a ...

, in

Coconino County Coconino County is a county in the north-central part of the U.S. state of Arizona. Its population was 145,101 at the 2020 census. The county seat is Flagstaff. The county takes its name from ''Cohonino'', a name applied to the Havasupai p ...

of northern

Arizona Arizona ( ; nv, Hoozdo Hahoodzo ; ood, Alĭ ṣonak ) is a U.S. state, state in the Southwestern United States. It is the list of U.S. states and territories by area, 6th largest and the list of U.S. states and territories by population, 14 ...

USA The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territor ...

. It is situated three miles south of the North Rim's Bright Angel Point, and towers 3,700 feet (1,130 meters) above Bright Angel Canyon. Its nearest higher neighbor is Brahma Temple, 1.5 mile to the south. Other neighbors include

Zoroaster Temple Zoroaster Temple is a summit located in the Grand Canyon, in Coconino County of Arizona, USA. It is situated northeast of the Yavapai Point overlook on the canyon's South Rim, from which it can be seen towering over above the Colorado River an ...

2.5 miles to the south-southwest,

Manu Temple Manu Temple is a 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, northeast of parent Buddha Temple, and three miles southwest of the No ...

three miles to the west-northwest, and

Buddha Temple Buddha Temple is a 7,212-foot-elevation (2,198 meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, in the Southwestern United States. It is situated 6.5 miles (10.5 km) due north of the Mather Point ...

, 3.5 miles to the west. Deva Temple was named by

Henry Gannett Henry Gannett (August 24, 1846 – November 5, 1914) was an American geographer who is described as the "father of mapmaking in America."Evans, Richard Tranter; Frye, Helen M. (2009).History of the Topographic Branch (Division) (PDF). ''U.S. Geo ...

, a geographer for

Clarence Dutton Clarence Edward Dutton (May 15, 1841 – January 4, 1912) was an American geologist and US Army officer. Dutton was born in Wallingford, Connecticut on May 15, 1841. He graduated from Yale College in 1860 and took postgraduate courses there un ...

, in following Dutton's practice of naming features in the Grand Canyon after mythological deities, in this case, Deva. This geographical feature's name was officially adopted in 1906 by the

U.S. Board on Geographic Names The United States Board on Geographic Names (BGN) is a federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geographic names throughout the federal govern ...

. According to the

Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, nota ...

system, Deva Temple is located in a

Cold semi-arid climate A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-a ...

zone.

Geology

The summit of Deva Temple is composed of cream-colored, cliff-forming,

Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Pale ...

Coconino Sandstone Coconino Sandstone is a geologic formation named after its exposure in Coconino County, Arizona. This formation spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. ...

with a small, remnant

Kaibab Limestone The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in Ar ...

caprock Caprock or cap rock is a more resistant rock type overlying a less resistant rock type,Kearey, Philip (2001). ''Dictionary of Geology'', 2nd ed., Penguin Reference, London, New York, etc., p. 41.. . analogous to an upper crust on a cake that is ha ...

. 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 The Permian Hermit Formation, also known as the Hermit Shale, is a nonresistant unit that is composed of slope-forming reddish brown siltstone, mudstone, and very fine-grained sandstone. Within the Grand Canyon region, the upper part of the H ...

, which in turn overlays the

Pennsylvanian Pennsylvanian may refer to: * A person or thing from Pennsylvania * Pennsylvanian (geology) The Pennsylvanian ( , also known as Upper Carboniferous or Late Carboniferous) is, in the International Commission on Stratigraphy, ICS geologic timesca ...

-Permian

Supai Group The Supai Group is a slope-forming section of red bed deposits found in the Colorado Plateau. The group was laid down during the Pennsylvanian to Lower Permian. Cliff-forming interbeds of sandstone are noticeable throughout the group. The Supai ...

. Further down are strata of

Mississippian Mississippian may refer to: * Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago *Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD ...

Redwall Limestone The Redwall Limestone is a resistant cliff-forming unit of Mississippian age that forms prominent, red-stained cliffs in the Grand Canyon, ranging in height from to . Lithology Redwall Limestone consists predominantly of light-olive-gray to ...

Cambrian The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ag ...

Tonto Group The Tonto Group is a name for an assemblage of related sedimentary strata, collectively known by geologists as a '' Group'', that comprises the basal sequence Paleozoic strata exposed in the sides of the Grand Canyon. As currently defined, the T ...

, and finally

Proterozoic The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided ...

Unkar Group The Unkar Group is a sequence of strata of Proterozoic age that are subdivided into five geologic formations and exposed within the Grand Canyon, Arizona, Southwestern United States. The 5-unit Unkar Group is the basal member of the 8-member G ...

at creek level.William Kenneth Hamblin, ''Anatomy of the Grand Canyon: Panoramas of the Canyon's Geology'', 2008, Grand Canyon Association Publisher, . Precipitation

runoff Runoff, run-off or RUNOFF may refer to: * RUNOFF, the first computer text-formatting program * Runoff or run-off, another name for bleed, printing that lies beyond the edges to which a printed sheet is trimmed * Runoff or run-off, a stock market ...

from Deva Temple drains south into the

Colorado River The Colorado River ( es, Río Colorado) is one of the principal rivers (along with the Rio Grande) in the Southwestern United States and northern Mexico. The river drains an expansive, arid watershed that encompasses parts of seven U.S. s ...

via

Bright Angel Creek Bright Angel Creek is an American body of water located at the bottom of the Grand Canyon National Park flowing into the Colorado River at the end of the North Kaibab Trail on the north side of the river. The creek originates from Roaring Sprin ...

on its west side, and Clear Creek on the east side.

Gallery

File:Bright Angel-temples.jpg, Deva Temple (left of center), Brahma and Zoroaster Temples (right) seen from the North Rim at Bright Angel Point File:Grand Canyon, Brahma Temple.jpg, Deva (left), Brahma (center), and Zoroaster Temples seen from North Rim File:Grand Canyon desde Grand Canyon lodge. 29.jpg, Deva Temple (left), Brahma Temple (right) File:Bright Angel Point.jpg, Deva Temple (left of center), Brahma and Zoroaster Temples (right) seen from the North Rim at Bright Angel Point File:Bright Angel, Deva and Angels Gate.jpg, Angels Gate (left) and Deva Temple (right) File:Deva Temple with Angels Gate.jpg,

Wotans Throne Wotans Throne is a summit located in the Grand Canyon, in Coconino County of Arizona, US. It is situated one mile immediately southwest of the Cape Royal overlook on the canyon's North Rim, 1.7 mile west-southwest of Freya Castle, two mil ...

, Angels Gate, and Deva Temple

References

External links

* Weather forecast
National Weather Service
{{Geology of the Grand Canyon area, , state=collapsed Grand Canyon Landforms of Coconino County, Arizona Mountains of Arizona Mountains of Coconino County, Arizona North American 2000 m summits Colorado Plateau Grand Canyon National Park Grand Canyon, North Rim Sandstone formations of the United States

Geology

Gallery

See also

References

External links