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Hancock Butte (Arizona)

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

Hancock Butte is a 7,683-foot-elevation (2,342-meter) summit located in the Grand Canyon, in Coconino County of northern Arizona, US.[2] It is situated one mile south of the Point Imperial viewpoint on the canyon's North Rim, where it towers 3,700 feet (1,100 meters) above Nankoweap Canyon. Its nearest higher neighbor is Mount Hayden, one mile to the north-northeast, Kibbey Butte is one mile to the south-southwest, and Brady Peak is 1.5 mile to the southeast. Hancock Butte is named after William A. Hancock (1831–1902), a pioneer and politician of the Arizona Territory known for performing the survey work required to create the town of Phoenix and erecting the first building there in 1870.[2] This geographical feature's name was officially adopted in 1932 by the U.S. Board on Geographic Names.[2] According to the Köppen climate classification system, Hancock Butte is located in a Cold semi-arid climate zone.[3]

Elevation7,683 ft (2,342 m)[1]
Prominence463 ft (141 m)[1]
Isolation0.81 mi (1.30 km)[1]
Quick facts Highest point, Elevation ...
Hancock Butte
North aspect centered, from Point Imperial
Highest point
Elevation7,683 ft (2,342 m)[1]
Prominence463 ft (141 m)[1]
Parent peakMount Hayden (8,362 ft)[1]
Isolation0.81 mi (1.30 km)[1]
Coordinates36°15′42″N 111°58′29″W[2]
Naming
EtymologyWilliam A. Hancock
Geography
Hancock Butte is located in Arizona
Hancock Butte
Hancock Butte
Location within Arizona
Hancock Butte is located in the United States
Hancock Butte
Hancock Butte
Location within the United States
Country
United States
State
Arizona
County
Coconino
Protected area
Grand Canyon National Park
Parent rangeKaibab Plateau
Colorado Plateau
Topo mapUSGS Point Imperial
Geology
Rock agePermian
Climbing
First ascentAlan Doty, October 1976
Easiest routeclass 5.1 climbing[1]
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Geology

Hancock Butte is a butte topped by Esplanade Sandstone, part of the Pennsylvanian-Permian Supai Group overlaying the cliff-forming Mississippian Redwall Limestone.[4] Precipitation runoff from this feature drains east into the Colorado River via Nankoweap Creek.

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