Earth:Geikie Peak

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Short description: Landform in the Grand Canyon, Arizona
Geikie Peak
 Geike Monument[1]
Aerial View of Geikie Peak.jpg
Aerial view of Geikie's east-southeast aspect.
(Scylla Butte lower right corner)
Highest point
Elevation5,005 ft (1,526 m) [2]
Prominence625 ft (191 m) [2]
Parent peakPeak 5180[2]
Isolation1.22 mi (1.96 km) [2]
Coordinates [ ⚑ ] : 36°08′00″N 112°16′09″W / 36.1334086°N 112.2691779°W / 36.1334086; -112.2691779 [1]
Naming
EtymologyArchibald Geikie
Geography
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LocationGrand Canyon National Park
Coconino County, Arizona, US
Parent rangeCoconino Plateau
Colorado Plateau
Topo mapUSGS Havasupai Point
Geology
Type of rocklimestone, shale, sandstone
Climbing
Easiest routeclass 5.4 climbing[2]

Geikie Peak is a 5,005-foot (1,526 m)-elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States.[1] It is situated nine miles (14 km) northwest of Grand Canyon Village, immediately north of Diana Temple, and south of Scorpion Ridge which lies across the opposite side of Granite Gorge. Access is via the Tonto Trail which traverses 270 degrees around the base of the peak. Topographic relief is significant as Geikie Peak rises over 2,600 feet (790 m) above the Colorado River in one-half mile (0.80 km). According to the Köppen climate classification system, Geikie Peak is located in a cold semi-arid climate zone.[3]

History

George Wharton James named it "Geikie Monument" in 1901 for Sir Archibald Geikie (1835–1924), Director General of the Geological Survey of the United Kingdom, who studied geology in the Grand Canyon, finding evidence to support his theories of erosion.[1] This feature's present name was officially adopted in 1908 by the U.S. Board on Geographic Names.

Sir Archibald Geikie

Geology

Geikie Peak is composed of Mississippian Redwall Limestone, with a small cupola of the basal layer of Pennsylvanian-Permian Supai Group on top. The cliff-forming Redwall overlays the Cambrian Tonto Group, and below that Paleoproterozoic Vishnu Basement Rocks at river level in Granite Gorge.[4][5]

Scylla Butte

At the end of Geikie Peak's east spur lies a smaller feature called Scylla Butte.[6] This feature is named for Scylla, a monster according to Greek mythology, in keeping with Clarence Dutton's practice of naming geographical features in the Grand Canyon after mythological deities.[7] It rises approximately 400 feet above the Tonto Trail which nearly surrounds it. The first ascent of this butte was made by James Kirshvink and James Ohlman on March 18, 1978.[8]

Scylla Butte, south aspect

See also

  • Geology of the Grand Canyon area

References

  1. ↑ 1.0 1.1 1.2 1.3 "Geikie Peak". United States Geological Survey. https://geonames.usgs.gov/apex/f?p=gnispq:3:::NO::P3_FID:4972. 
  2. ↑ 2.0 2.1 2.2 2.3 2.4 "Geikie Peak – 5,995' AZ". https://listsofjohn.com/peak/75534. 
  3. ↑ 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. 
  4. ↑ N.H. Darton, Story of the Grand Canyon of Arizona, 1917, page 12.
  5. ↑ William Kenneth Hamblin, Anatomy of the Grand Canyon: Panoramas of the Canyon's Geology, 2008, Grand Canyon Association Publisher, ISBN:9781934656013.
  6. ↑ "Scylla Butte". United States Geological Survey. https://geonames.usgs.gov/apex/f?p=gnispq:3:::NO::P3_FID:11032. 
  7. ↑ Randy Moore and Kara Felicia Witt, The Grand Canyon: An Encyclopedia of Geography, History, and Culture, 2018, ABC-CLIO Publisher, page 151.
  8. ↑ Aaron Tomasi, Pernell Tomasi, Grand Canyon Summits Select An Obscure Compilation of Sixty-nine Remote Ascent Routes in the Grand Canyon National Park Backcountry, 2001, ISBN:9780971088009, page 81.
Grand Canyon aerial, Geikie Peak lower left, Scorpion Ridge to right

External links



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