Manu Temple facts for kids

Quick facts for kids Manu Temple
Manu Temple centered, south aspect (Buddha Temple left, Oza Butte upper right)
Highest point
Elevation	7,184 ft (2,190 m)
Prominence	524 ft (160 m)
Isolation	1.26 mi (2.03 km)
Parent peak	Buddha Temple (7,212 ft)
Geography
Manu Temple Location in Arizona Show map of Arizona Manu Temple Location in the United States Show map of the United States
Location	Grand Canyon National Park Coconino County, Arizona, US
Parent range	Kaibab Plateau Colorado Plateau
Topo map	USGS Bright Angel Point
Type of rock	sandstone, limestone, mudstone
Climbing
Easiest route	class 4 climbing

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 mile (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 (1,100 meters) 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.

Manu Temple was named by George Wharton James for the Hindu lawgiver Manu, in keeping with Clarence Dutton's practice of naming features in the Grand Canyon after mythological deities. This geographical feature's name was officially adopted in 1906 by the U.S. Board on Geographic Names.

According to the Köppen climate classification system, Manu Temple is located in a Cold semi-arid climate zone. Precipitation runoff from Manu Temple drains south into the Colorado River via Bright Angel Creek on its east side, and Phantom Creek on the west side.

Geology

The summit of Manu Temple is composed of cream-colored, cliff-forming, Permian Coconino Sandstone, which is the third-youngest of the strata in the Grand Canyon, and 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.

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