Marble Canyon
{{short description|Section of the Colorado River in Arizona}}
{{Other places}}
{{Infobox valley
|name = Marble Canyon
|photo = Canyon midday.jpg
|photo_caption = A section of Marble Canyon from river level
|coordinates = {{coord|36.863622|N|111.590152|W|type:landmark_region:US-AZ|format=dms|display=inline,title}}
}}
Marble Canyon is the section of the Colorado River canyon in northern Arizona from Lee's Ferry to the confluence with the Little Colorado River, which marks the beginning of the Grand Canyon.
Lee's Ferry is a common launching point for river runners starting their journey through Marble Canyon and then onward to the Grand Canyon. Marble Canyon is also well known for the Navajo Bridge, where US Highway 89A crosses the Colorado River.
Marble Canyon marks the western boundary of the Navajo Nation. In 1975, the former Marble Canyon National Monument, which followed the Colorado River northeast from the Grand Canyon to Lee's Ferry, was made part of Grand Canyon National Park.
Image:'Noon Day Rest in Marble Canyon' from the second Powell Expedition 1872.jpg's second expedition on a noon-day rest in Marble Canyon]]
The name Marble Canyon is a misnomer because there is no marble there. Although John Wesley Powell knew this when he named the canyon, he thought the polished limestone looked like marble. In his words, "The limestone of the canyon is often polished, and makes a beautiful marble. Sometimes the rocks are of many colors – white, gray, pink, and purple, with saffron tints."
Marble Canyon is the site of one of the last great proposed dam projects on the Colorado, the Marble Canyon Dam. Proposed and investigated in the early 1950s by the United States Bureau of Reclamation,Glenn Rink, Grand Canyon River Guides BQR, [http://www.gcrg.org/bqr/10-2/mcd.html Life at the Marble Canyon Damsites] {{Webarchive|url=https://web.archive.org/web/20080830025940/http://www.gcrg.org/bqr/10-2/mcd.html |date=2008-08-30 }}, spring 1997. Retrieved May 16, 2007. the proposal met substantial opposition, notably from the Sierra Club, when a revived proposal was considered by the state of Arizona as part of the Central Arizona Project from 1965 to 1968. The proposed dam was finally abandoned in 1968. Exploratory holes, which were drilled in the Redwall Limestone of the canyon walls in an early phase of the abortive project, can still be seen at Mile 39.2.Mesa Community College, [http://www.physci.mc.maricopa.edu/Geology/FieldTrips/ColoradoRiver/2004Summer/ColoradoRiver_su04_Images_Day02.htm Geology Field Trip: Colorado River] {{webarchive|url=https://web.archive.org/web/20060907031201/http://www.physci.mc.maricopa.edu/Geology/FieldTrips/ColoradoRiver/2004Summer/ColoradoRiver_su04_Images_Day02.htm |date=2006-09-07 }}, Summer 2004. Retrieved May 16, 2007.
Image:Marble Canyon from Navajo Bridge panorama.jpg.]]
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Geology
The uppermost walls of Marble Canyon are composed of Kaibab Limestone upon the Toroweap Formation upon Coconino Sandstone.Geology of the Lees Ferry area Coconino County, Arizona, Geological Survey Bulletin 1137, 1963, pp. 8–9, labeled map p. 9.
Ecology
Marble Canyon is the only home of the endangered cactus Pediocactus bradyi. [http://www.natureserve.org/explorer/servlet/NatureServe?searchName=Pediocactus+bradyi Pediocactus bradyi.] The Nature Conservancy. The critically endangered California Condor occurs in Marble Canyon. [https://aziba.org/?page_id=476] Arizona Important Bird Areas Program.
References
{{Reflist}}
External links
{{commons category|Marble Canyon}}
- [https://grcahistory.org/sites/colorado-river-corridor/marble-canyon/ Marble Canyon – Nature, culture, & history; “GrandCaHistory.org”]
{{Colorado River system}}
{{Authority control}}
Category:Canyons and gorges of Arizona