Cheops Pyramid

Landform in the Grand Canyon, Arizona From Wikipedia, the free encyclopedia

Cheops Pyramid is a 5,401-foot-elevation (1,646-meter) summit located in the Grand Canyon, in Coconino County of Arizona, US.[3]

Elevation5,401 ft (1,646 m)[1]
Prominence800 ft (240 m)[1]
Isolation1.72 mi (2.77 km)[2]
Quick facts Highest point, Elevation ...
Cheops Pyramid
South aspect, from South Rim's Yavapai Point
Highest point
Elevation5,401 ft (1,646 m)[1]
Prominence800 ft (240 m)[1]
Parent peakIsis Temple (7,006 ft)[2]
Isolation1.72 mi (2.77 km)[2]
Coordinates36°07′13″N 112°07′12″W[3]
Geography
Cheops Pyramid is located in Arizona
Cheops Pyramid
Cheops Pyramid
Location in Arizona
Cheops Pyramid is located in the United States
Cheops Pyramid
Cheops Pyramid
Cheops Pyramid (the United States)
CountryUnited States
StateArizona
CountyCoconino
Protected areaGrand Canyon National Park
Parent rangeKaibab Plateau[1]
Colorado Plateau
Topo mapUSGS Phantom Ranch
Geology
Rock type(s)sandstone, limestone, shale
Climbing
Easiest routeclass 4 climbing[2]
Close

Description

This butte is situated four miles north of Grand Canyon Village, 2.5 miles south-southwest of Buddha Temple, and 1.7 mile south-southeast of Isis Temple, which is the nearest higher neighbor. Topographic relief is significant as it rises 3,000 feet (910 meters) above the Colorado River in 1.5 mile. It was named by George Wharton James for the fanciful resemblance to the famous pyramid constructed by Egyptian Pharaoh Cheops.[4] This was in keeping with Clarence Dutton's tradition of naming geographical features in the Grand Canyon after mythological deities.[5] This butte's toponym was officially adopted in 1906 by the U.S. Board on Geographic Names.[3] According to the Köppen climate classification system, Cheops Pyramid is located in a Cold semi-arid climate zone.[6]

Geology

Cheops Pyramid is a flat-topped erosional remnant composed of Mississippian Redwall Limestone, overlaying the green shale slopes of the Cambrian Tonto Group, and below that red shale and Shinumo Quartzite of the Proterozoic Unkar Group.[7] Precipitation runoff from Cheops Pyramid drains south to the Colorado River via Phantom Creek (east), and Ninetyone Mile Creek (west).

See also

References

Related Articles

Wikiwand AI