Gila River: Difference between revisions
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{{Short description|River in New Mexico and Arizona, United States}} |
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{{Infobox river |
{{Infobox river |
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| name = Gila River |
| name = Gila River |
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| subdivision_type2 = State |
| subdivision_type2 = State |
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| subdivision_name2 = [[Arizona]] |
| subdivision_name2 = [[Arizona]] |
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| subdivision_type3 = State |
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| subdivision_name3 = [[New Mexico]] |
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| subdivision_type4 = |
| subdivision_type4 = |
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| subdivision_name4 = |
| subdivision_name4 = |
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| depth_avg = |
| depth_avg = |
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| depth_max = |
| depth_max = |
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| discharge1_location= [[Dome, Arizona|Dome, AZ]]; {{convert|12|mi|km|abbr=on}} from the mouth<ref name="discharge">{{cite web|url=http://wdr.water.usgs.gov/wy2011/pdfs/09520500.2011.pdf|title=USGS Gage #09520500 on the Gila River near Dome, AZ|publisher=U.S. Geological Survey|work=National Water Information System|date=1903–2011| |
| discharge1_location= [[Dome, Arizona|Dome, AZ]]; {{convert|12|mi|km|abbr=on}} from the mouth<ref name="discharge">{{cite web|url=http://wdr.water.usgs.gov/wy2011/pdfs/09520500.2011.pdf|title=USGS Gage #09520500 on the Gila River near Dome, AZ|publisher=U.S. Geological Survey|work=National Water Information System|date=1903–2011|access-date=2012-03-16}}</ref> |
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| discharge1_min = {{convert|0|cuft/s|m3/s|abbr=on}} |
| discharge1_min = {{convert|0|cuft/s|m3/s|abbr=on}} |
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| discharge1_avg = {{convert|247|cuft/s|m3/s|abbr=on}}<ref name="discharge" |
| discharge1_avg = {{convert|247|cuft/s|m3/s|abbr=on}}<ref name="discharge" /> |
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| discharge1_max = {{convert|200000|cuft/s|m3/s|abbr=on}} |
| discharge1_max = {{convert|200000|cuft/s|m3/s|abbr=on}} |
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<!---------------------- BASIN FEATURES --> |
<!---------------------- BASIN FEATURES --> |
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| source1 = Confluence of East and West Forks |
| source1 = Confluence of East and West Forks |
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| source1_location = [[Grant County, New Mexico|Grant County]], [[New Mexico]] |
| source1_location = [[Grant County, New Mexico|Grant County]], [[New Mexico]] |
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| source1_coordinates= {{coord|33|10|47|N|108|12|22|W|display=inline}}<ref name="GNIS">{{cite gnis|id=42838|name=Gila River|entrydate=1980-02-08| |
| source1_coordinates= {{coord|33|10|47|N|108|12|22|W|display=inline}}<ref name="GNIS">{{cite gnis|id=42838|name=Gila River|entrydate=1980-02-08|access-date=2012-03-16}}</ref> |
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| source1_elevation = {{convert|5551|ft|abbr=on}} |
| source1_elevation = {{convert|5551|ft|abbr=on}} |
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| mouth = [[Colorado River]] |
| mouth = [[Colorado River]] |
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| basin_size = {{convert|58200|sqmi|abbr=on}}<ref name="USGSrivers"/> |
| basin_size = {{convert|58200|sqmi|abbr=on}}<ref name="USGSrivers"/> |
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| tributaries_left = [[San Simon River (Arizona)|San Simon River]], [[San Pedro River (Arizona)|San Pedro River]], [[Santa Cruz River (Arizona)|Santa Cruz River]] |
| tributaries_left = [[San Simon River (Arizona)|San Simon River]], [[San Pedro River (Arizona)|San Pedro River]], [[Santa Cruz River (Arizona)|Santa Cruz River]] |
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| tributaries_right = [[San Francisco River]], [[Salt River (Arizona)|Salt River]], [[Agua Fria River]], [[Hassayampa River]] |
| tributaries_right = [[San Francisco River (central Arizona)|San Francisco River]], [[Salt River (Arizona)|Salt River]], [[Agua Fria River]], [[Hassayampa River]] |
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| custom_label = |
| custom_label = |
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| custom_data = |
| custom_data = |
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| extra = {{Infobox mapframe |wikidata=yes |zoom=5 |height=250 | stroke-width=1.5 |coord {{WikidataCoord|display=i}}}} |
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| extra = |
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}} |
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The '''Gila River''' ({{IPAc-en|ˈ|h|iː|l|ə}}; [[O'odham language|O'odham [Pima]]]: '''Keli Akimel''' or simply '''Akimel''', [[Quechan language|Quechan]]: '''Haa Siʼil''') is a {{convert|649|mi|km|adj= |
The '''Gila River''' ({{IPAc-en|ˈ|h|iː|l|ə}}; [[O'odham language|O'odham [Pima]]]: '''Keli Akimel''' or simply '''Akimel''', [[Quechan language|Quechan]]: '''Haa Siʼil''', [[Maricopa language]]: '''Xiil'''<ref>Antone, Caroline. ''Piipayk m'iim''. Salt River: Oʼodham Piipaash Language Program, 2000.</ref>) is a {{convert|649|mi|km|adj=mid|-long}}<ref name="USGSrivers">{{cite web|url= http://pubs.usgs.gov/of/1987/ofr87-242/|author=Kammerer, J.C.|title=Largest Rivers in the United States|publisher=U.S. Geological Survey |access-date=2012-03-16}}</ref> [[tributary]] of the [[Colorado River]] flowing through [[New Mexico]] and [[Arizona]] in the United States. The river drains an arid watershed of nearly {{convert|60000|mi2|km2}} that lies mostly within the U.S., but also extends into northern [[Sonora]], Mexico. |
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Indigenous peoples have lived along the river for at least 2,000 years, establishing complex agricultural societies before European exploration of the region began in the 16th century. [[European Americans]] did not permanently settle the Gila River watershed until the mid-19th century. |
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⚫ | During the 20th century, |
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⚫ | During the 20th century, development in the Gila River watershed prompted the construction of large diversion and flood control structures on the river and its tributaries, and consequently the Gila contributes only a small fraction of its historic flow to the Colorado.<ref>"The Gila is mostly bone dry in its lower reaches" (Jonathan Waterman, "American Nile: Saving the Colorado", ''National Geographic'').</ref> The historic natural discharge of the river was around {{convert|1900|cuft/s}}, but has declined to only {{convert|247|cuft/s}}. The engineering projects transformed much of the river valley and its surroundings from arid desert into irrigated land, and supply water to more than five million people in the [[Phoenix metropolitan area|Phoenix]] and [[Pima County|Tucson]] metropolitan areas who live in the watershed. |
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==Geography== |
==Geography== |
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The Gila River has its source in western New Mexico, in [[Sierra County, New Mexico|Sierra County]] on the western slopes of [[Continental Divide]] in the [[Black Range]]. It flows southwest through the [[Gila National Forest]] |
The Gila River has its source in western New Mexico, in [[Sierra County, New Mexico|Sierra County]] on the western slopes of the [[Continental Divide]] in the [[Black Range]]. It flows southwest through the [[Gila National Forest]], the Gila Wilderness, and [[Gila Cliff Dwellings National Monument]], then westward into Arizona, past the town of [[Safford, Arizona|Safford]]. After flowing along the southern slope of the [[Gila Mountains (Graham County)|Gila Mountains]] in [[Graham County, Arizona|Graham County]] through a series of canyons, the Gila is impounded by [[Coolidge Dam]] in [[San Carlos Lake]] south of [[Peridot, Arizona|Peridot]]. |
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It emerges from the mountains into the valley southeast of Phoenix, Arizona, where it crosses the [[Gila River Indian Reservation]] as an intermittent [[stream]] due to large [[irrigation]] diversions. Well west of Phoenix, the river bends sharply southward along the Gila Bend Mountains, then it swings westward again near the town of [[Gila Bend, Arizona|Gila Bend]]. It flows southwestward between the [[Gila Mountains (Yuma County)|Gila Mountains]] to the south and the [[Laguna Mountains (Arizona)|Languna]] and [[Muggins Mountains|Muggins]] ranges to the north in [[Yuma County, Arizona|Yuma County]], and finally it empties into the Colorado at [[Yuma, Arizona]]. |
It emerges from the mountains into the valley southeast of Phoenix, Arizona, where it crosses the [[Gila River Indian Reservation]] as an intermittent [[stream]] due to large [[irrigation]] diversions, primarily at the Hayden Ashurst Diversion Dam. Well west of Phoenix, the river bends sharply southward along the Gila Bend Mountains, then it swings westward again near the town of [[Gila Bend, Arizona|Gila Bend]]. It flows southwestward between the [[Gila Mountains (Yuma County)|Gila Mountains]] to the south and the [[Laguna Mountains (Arizona)|Languna]] and [[Muggins Mountains|Muggins]] ranges to the north in [[Yuma County, Arizona|Yuma County]], and finally it empties into the Colorado at [[Yuma, Arizona]]. |
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The Gila is joined by many tributaries, beginning with the East and West Forks of the river, which combine to form the main stem near Gila Hot Springs in New Mexico. Above Safford, it is joined by the [[San Francisco River]] and the intermittent San Simon River. Further downstream, it is joined by the San Carlos River from the north in San Carlos Lake. At [[Winkelman, Arizona]], it picks up the [[San Pedro River (Arizona)|San Pedro River]] and then is joined by the [[Santa Cruz River (Arizona)|Santa Cruz River]] south of [[Casa Grande, Arizona|Casa Grande]]. The [[Salt River (Arizona)|Salt River]], its main tributary, joins in the Phoenix metropolitan area, and further west the Gila receives its last two major tributaries, the [[Agua Fria River|Agua Fria]] and [[Hassayampa River|Hassayampa]] Rivers, from the north. |
The Gila is joined by many tributaries, beginning with the East and West Forks of the river, which combine to form the main stem near [[Gila Hot Springs, New Mexico|Gila Hot Springs]] in New Mexico. Above Safford, it is joined by the [[San Francisco River (central Arizona)|San Francisco River]] and the intermittent San Simon River. Further downstream, it is joined by the San Carlos River from the north in San Carlos Lake. At [[Winkelman, Arizona]], it picks up the [[San Pedro River (Arizona)|San Pedro River]] and then is joined by the [[Santa Cruz River (Arizona)|Santa Cruz River]] south of [[Casa Grande, Arizona|Casa Grande]]. The [[Salt River (Arizona)|Salt River]], its main tributary, joins in the Phoenix metropolitan area, and further west the Gila receives its last two major tributaries, the [[Agua Fria River|Agua Fria]] and [[Hassayampa River|Hassayampa]] Rivers, from the north. |
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Although the Gila River flows entirely within the United States, the headwaters of two tributaries – the San Pedro and [[Santa Cruz River (Arizona)|Santa Cruz]] Rivers – extend into Mexico. About {{convert|1630|mi2|km2|abbr=on}}, or 2.8% of the Gila's {{convert|58200|mi2|km2|adj=on}} watershed, is in Mexico.<ref name="USGSbasins">{{cite web|title=Boundary Descriptions and Names of Regions, Subregions, Accounting Units and Cataloging Units |url=http://water.usgs.gov/GIS/huc_name.html |publisher=U.S. Geological Survey | |
Although the Gila River flows entirely within the United States, the headwaters of two tributaries – the San Pedro and [[Santa Cruz River (Arizona)|Santa Cruz]] Rivers – extend into Mexico. About {{convert|1630|mi2|km2|abbr=on}}, or 2.8% of the Gila's {{convert|58200|mi2|km2|adj=on}} watershed, is in Mexico.<ref name="USGSbasins">{{cite web|title=Boundary Descriptions and Names of Regions, Subregions, Accounting Units and Cataloging Units |url=http://water.usgs.gov/GIS/huc_name.html |publisher=U.S. Geological Survey |access-date=2012-03-16}}</ref> A further {{convert|3300|mi2|km2|abbr=on}} or 5.7% lies within New Mexico, while the remaining majority, {{convert|53270|mi2|km2|abbr=on}} or 91.5%, is in Arizona.<ref>{{cite web|url=http://wdr.water.usgs.gov/wy2011/pdfs/09432000.2011.pdf|title=USGS Gage #09432000 on the Gila River Below Blue Creek, Near Virden, NM|publisher=U.S. Geological Survey|work=National Water Information System|date=1914–2011|access-date=2012-03-16|archive-url=https://web.archive.org/web/20130720110629/http://wdr.water.usgs.gov/wy2011/pdfs/09432000.2011.pdf|archive-date=2013-07-20|url-status=dead}}</ref> |
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==History== |
==History== |
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⚫ | A band of [[Pima people|Pima]] (autonym "Akimel O'odham", river people), the Keli Akimel O'odham (Gila River People), have lived on the banks of the Gila River since before the arrival of Spanish explorers. Popular theory says that the word "Gila" was derived from a Spanish contraction of Hah-quah-sa-eel, a [[Yuma language|Yuma]] word meaning "running water which is salty".<ref>{{cite web|url=http://www2.srs.fs.fed.us/r3/gila/about/ |title=Gila National Forest (archived) |publisher=[[United States Forest Service]] |date=2003-12-04 |access-date=2007-10-16 |url-status=dead |archive-url=https://web.archive.org/web/20060111100317/http://www2.srs.fs.fed.us/r3/gila/about/ |archive-date=January 11, 2006 }}</ref> Their traditional way of life (''himdagĭ'', sometimes rendered in English as Him-dak) was and is centered at the river, which is considered holy. Traditionally, sand from the banks of the river is used as an exfoliant when bathing (often in rainstorms, especially during the monsoon). |
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⚫ | Indigenous peoples such as the [[Hohokam]] were responsible for creating large, complex civilizations along the Middle Gila River and Salt River between 600 and 1450 AD. These native civilizations depended largely on irrigated agriculture, for which they constructed over {{convert|200|mi|km}} of canals.<ref>{{cite web|url=http://www.waterhistory.org/histories/hohokam2/|title=Hohokam Legacy: Desert Canals|publisher=WaterHistory.org|work=Pueblo Grande Museum Profiles No. 12|author=Howard, Jerry B.|access-date=2012-03-16|archive-url=https://web.archive.org/web/20120124025948/http://www.waterhistory.org/histories/hohokam2/|archive-date=2012-01-24|url-status=dead}}</ref> The upper Gila was inhabited by the [[Mogollon culture]] over most of the same time period, in settlements like those at [[Gila Cliff Dwellings National Monument]] in the later period. |
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⚫ | A band of [[Pima people|Pima]] (autonym "Akimel O'odham", river people), the Keli Akimel O'odham (Gila River People), have lived on the banks of the Gila River since before the arrival of Spanish explorers. Popular theory says that the word "Gila" was derived from a Spanish contraction of Hah-quah-sa-eel, a [[Yuma language|Yuma]] word meaning "running water which is salty".<ref>{{cite web|url=http://www2.srs.fs.fed.us/r3/gila/about/ |title=Gila National Forest (archived) |publisher=[[United States Forest Service]] |date=2003-12-04 | |
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⚫ | Indigenous peoples such as the [[Hohokam]] were responsible for creating large, complex civilizations along the Middle Gila River and Salt River between 600 and 1450 AD. These native civilizations depended largely on irrigated agriculture, for which they constructed over {{convert|200|mi|km}} of canals.<ref>{{cite web|url=http://www.waterhistory.org/histories/hohokam2/|title=Hohokam Legacy: Desert Canals|publisher=WaterHistory.org|work=Pueblo Grande Museum Profiles No. 12|author=Howard, Jerry B.|date |
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The first European to see the Gila River was possibly [[Spain|Spanish]] explorer and missionary [[Juan de la Asunción]]. Asunción reached the Gila in 1538 after traveling northwards along one of its tributaries, either the San Pedro or Santa Cruz.<ref>{{cite journal|author1=Hartmann, William K. |author2=Hartmann, Gayle Harrison |title=Juan de la Asunción, 1538: First Spanish Explorer of Arizona?|journal=Kiva|volume=37|number=2|year=1972|pages=93–103|doi=10.1080/00231940.1972.11757756 }}</ref> In 1540, [[Hernando de Alarcón]] sailed up the Colorado and Gila Rivers; maps drawn by his expedition show the river as the ''Miraflores'' or ''Brazos de la Miraflores''.<ref>{{cite web|url=http://southwest.library.arizona.edu/reaz/body.1_div.5.html|title=Rivers and Mountains|publisher=University of Arizona|work=Books of the Southwest|date |
The first European to see the Gila River was possibly [[Spain|Spanish]] explorer and missionary [[Juan de la Asunción]]. Asunción reached the Gila in 1538 after traveling northwards along one of its tributaries, either the San Pedro or Santa Cruz.<ref>{{cite journal|author1=Hartmann, William K. |author2=Hartmann, Gayle Harrison |title=Juan de la Asunción, 1538: First Spanish Explorer of Arizona?|journal=Kiva|volume=37|number=2|year=1972|pages=93–103|doi=10.1080/00231940.1972.11757756 }}</ref> In 1540, [[Hernando de Alarcón]] sailed up the Colorado and Gila Rivers; maps drawn by his expedition show the river as the ''Miraflores'' or ''Brazos de la Miraflores''.<ref>{{cite web|url=http://southwest.library.arizona.edu/reaz/body.1_div.5.html|title=Rivers and Mountains|publisher=University of Arizona|work=Books of the Southwest|access-date=2012-03-16|archive-url=https://web.archive.org/web/20100709175820/http://southwest.library.arizona.edu/reaz/body.1_div.5.html|archive-date=2010-07-09|url-status=dead}}</ref> |
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⚫ | During the [[Mexican–American War]], General [[Stephen Watts Kearny]] marched 100 cavalrymen from the [[1st U.S. Dragoons]] along the Gila River in November 1846.<ref>{{cite book|last=Turner|first=Henry Smith|title=The original journals of Henry Smith Turner with Stephen Watts Kearny to New Mexico and California, 1846–1847. Edited and with an introd. by Dwight L. Clarke.|year=1966|publisher=University of Oklahoma Press|location=Norman|page=87}}</ref> This detachment was guided by [[Kit Carson]]. The [[Mormon Battalion]] followed Kearny's troops, building a wagon trail roughly following the river from December 1846 to January 1847.<ref>{{cite book|last=Tyler|first=Daniel|title=A Concise History of the Mormon Battalion in the Mexican War, 1846–1847|url=https://archive.org/details/mormonbattalion0000unse|url-access=registration|year=1969|publisher=Rio Grande Press|location=Glorieta, NM|page=[https://archive.org/details/mormonbattalion0000unse/page/233 233]|isbn=978-0873800112}}</ref> |
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⚫ | After the [[Treaty of Guadalupe-Hidalgo]] in 1848, the Gila River served as a part of the border between the United States and Mexico until the 1853 [[Gadsden Purchase]] extended American territory well south of the Gila. The confluence of the Gila with the Colorado River was also used as a reference point for the southern border of California. Beginning in 1871, mainly [[Mormon]] settlers populated the Gila River valley around modern Phoenix, using the Gila, Salt, and San Pedro Rivers for irrigation and establishing at least six major settlements.<ref>{{cite web|url=http://www.lightplanet.com/mormons/daily/history/gathering/Arizona_EOM.htm|title=Pioneer Settlements in Arizona|author=Peterson, Charles S.|publisher=Light Planet|year=1992|access-date=2012-03-16|archive-url=https://web.archive.org/web/20120220004602/http://www.lightplanet.com/mormons/daily/history/gathering/Arizona_EOM.htm|archive-date=2012-02-20|url-status=dead}}</ref> |
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⚫ | During the [[Mexican–American War]], General [[Stephen Watts Kearny]] marched 100 cavalrymen from the [[1st U.S. Dragoons]] along the Gila River in November 1846.<ref>{{cite book|last=Turner|first=Henry Smith|title=The original journals of Henry Smith Turner with Stephen Watts Kearny to New Mexico and California, |
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⚫ | In 1944, 25 German [[prisoner of war|prisoners of war]] pulled off the [[Great Papago Escape|largest and most spectacular escape]] from an American compound during the war, digging a {{convert|178|ft|m|adj=on}} tunnel out of the Navy’s [[Papago Park]] Prisoner of War Camp in Arizona. All of the men were eventually captured, though some remained at large for more than a month. Among the last to be captured were three German soldiers who had based their audacious but ill-fated escape plans on a stolen highway map of Arizona, which showed the Gila River leading to the Colorado River, which in turn led to Mexico. Devising a scheme to flee by water, the Germans constructed a collapsible [[kayak]] under the noses of their American captors, tested it in a makeshift pool within the prison compound, then sneaked it out through the tunnel. Their plan was perfect – except for the map. The Gila, shown as a healthy blue waterway, turned out to be little more than a dry rut.<ref>Harvey, Miles, 2000, ''The Island of Lost Maps''. p. 154.{{ISBN?}}</ref> |
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⚫ | After the [[Treaty of Guadalupe-Hidalgo]] in 1848, the Gila River served as a part of the border between the United States and Mexico until the 1853 [[Gadsden Purchase]] |
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<gallery widths="200px" heights="155px"> |
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⚫ | In 1944, 25 German [[prisoner of war|prisoners of war]] pulled off the [[Great Papago Escape|largest and most spectacular escape]] from an American compound during the war, digging a {{convert|178|ft|m|adj=on}} tunnel out of the Navy’s [[Papago Park]] Prisoner of War Camp in Arizona. All of the men were eventually captured, though some remained at large for more than a month. Among the last to be captured were three German soldiers who had based their audacious but ill-fated escape plans on a stolen highway map of Arizona, which showed the Gila River leading to the Colorado River, which in turn led to Mexico. Devising a scheme to flee by water, the Germans constructed a collapsible [[kayak]] under the noses of their American captors, tested it in a makeshift pool within the prison compound, then sneaked it out through the tunnel. Their plan was perfect – except for the map. The Gila, shown as a healthy blue waterway, turned out to be little more than a dry rut.<ref>Harvey, Miles, 2000, The Island of Lost Maps. |
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⚫ | File:McPhaul Suspension Bridge.jpg|The [[McPhaul Suspension Bridge]] on a former section of [[US Route 95]] spans the Gila between the [[Gila Mountains (Yuma County)|Gila]] and [[Laguna Mountains (Arizona)|Laguna]] ranges in Yuma County. The bridge is listed on the [[National Register of Historic Places]]. |
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</gallery> |
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==Hydrology== |
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==Dams and diversions== |
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The only major dam on the Gila River is Coolidge Dam, {{convert|31|mi|km}} southeast of [[Globe, Arizona]], which forms San Carlos Lake. The [[Painted Rock Dam]] crosses the Gila near Gila Bend, although the river is |
The only major dam on the Gila River is Coolidge Dam, {{convert|31|mi|km}} southeast of [[Globe, Arizona]], which forms San Carlos Lake. The [[Painted Rock Dam]] crosses the Gila near Gila Bend, although the river is intermittent at that point. The majority of the water is diverted at the Ashurst-Hayden Diversion Dam near [[Florence, Arizona]]. A number of minor [[diversion dam]]s have been built on the river between the Painted Rock Dam and the Coolidge Dam, including the [[Gillespie Dam]], which was breached during a flood in 1993. |
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Many dams have been built on tributaries to the Gila River, including [[Theodore Roosevelt Dam]], [[Horse Mesa Dam]], and [[Mormon Flat Dam]] on the [[Salt River (Arizona)|Salt River]], [[New Waddell Dam]] on the [[Agua Fria River]], and [[Bartlett Dam]] on the [[Verde River]]. |
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The Gila River and its main tributary, the Salt River, would both be perennial streams carrying large volumes of water, but irrigation and municipal water diversions turn both into usually dry rivers. Below Phoenix to the Colorado River, the Gila is usually either a trickle or completely dry, as is also the lower Salt from [[Granite Reef Diversion Dam]] downstream to the Gila, but both rivers can carry large volumes of water following rainfall. A long time ago, the Gila River was navigable by large riverboats from its mouth to near Phoenix, and by smaller craft from Phoenix nearly to the Arizona – New Mexico border. The width varied from {{convert|150|to|1200|ft|m}} with a depth of {{convert|2|to|40|ft|m}}. The natural discharge of the river was roughly {{convert|1300000|acre feet|km3}} per year, with a mean flow of about {{convert|1800|cuft/s|m3/s}} at the mouth.<ref>{{cite journal |
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|authors=Cohen, Michael J.; Henges-Jeck, Christine; Castillo-Moreno, Gerardo |
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Many major dams in the Gila River system were built and operated by the [[U.S. Bureau of Reclamation]], which also constructed most of the large dams throughout the Colorado River basin. Others, such as Coolidge Dam, are owned by local water supply agencies, irrigation districts, or Native American tribes. |
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The Gila River and its main tributary, the Salt River, were both perennial streams carrying large volumes of water – the Gila was once navigable by large riverboats from its mouth to near Phoenix, and by smaller craft from Phoenix nearly to the Arizona-New Mexico border – until irrigation and municipal water diversions turned both into usually dry rivers which carry water only after local downpours create flooding. Below Phoenix to the Colorado River, the Gila is usually either a trickle or completely dry, as is also the lower Salt from [[Granite Reef Diversion Dam]] downstream to the Gila, but both rivers can carry large volumes of water following rainfall. |
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The historic width of the Gila River varied from {{convert|150|to|1200|ft|m}} with a depth of {{convert|2|to|40|ft|m}}. Its natural discharge was roughly {{convert|1300000|acre feet|km3}} per year, with a mean flow of about {{convert|1800|cuft/s|m3/s}} at the mouth.<ref>{{cite journal |
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|journal=Journal of Arid Environments |
|journal=Journal of Arid Environments |
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|year=2001 |
|year=2001 |
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|volume=49 |
|volume=49 |
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|issue=1 |
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|pages=35–48 |
|pages=35–48 |
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|doi=10.1006/jare.2001.0834 |bibcode=2001JArEn..49...35C |
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}}</ref> The river's modern discharge near the mouth is less than {{convert|180000|acre feet|km3}} per year, with an average flow of just {{convert|247|cuft/s|m3/s}}.<ref name="discharge"/> Overdraft from the Gila River system prompted the construction of the [[Central Arizona Project]], which delivers some {{convert|1500000|acre feet|km3}} annually from the Colorado River to supplement water supplies in the basin.<ref>{{cite web|url=http://www.usbr.gov/lc/phoenix/biology/azfish/biologicalop.html|title=Biological Opinion on the Transportation and Delivery of Central Arizona Project Water to the Gila River Basin in Arizona and New Mexico|publisher=U.S. Bureau of Reclamation|work=Native Aquatic Species of the Gila River Basin in Arizona and New Mexico|date=2010-08-30|access-date=2012-03-18}}</ref> |
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The upper Gila River, including its entire length within New Mexico, is a free-flowing one. Recent efforts to allow for damming or otherwise diverting this stretch have met with stiff political resistance, having been named as one of the nation's most endangered rivers due to proposed dam projects such as [[Hooker Dam]]. During his time in office, former New Mexico Governor [[Bill Richardson]] had promised to block any such attempt during his term, and he had even considered pushing for a statutory prohibition against any such projects on the state's portion of the river.<ref>{{cite news|url=http://www.lcsun-news.com/ci_8960289|title=NM governor pledges to fight Gila River diversion|last=Massey|first=Barry|date=2008-04-17| |
The upper Gila River, including its entire length within New Mexico, is a free-flowing one. Recent efforts to allow for damming or otherwise diverting this stretch have met with stiff political resistance, having been named as one of the nation's most endangered rivers due to proposed dam projects such as [[Hooker Dam]]. During his time in office, former New Mexico Governor [[Bill Richardson]] had promised to block any such attempt during his term, and he had even considered pushing for a statutory prohibition against any such projects on the state's portion of the river.<ref>{{cite news|url=http://www.lcsun-news.com/ci_8960289|title=NM governor pledges to fight Gila River diversion|last=Massey|first=Barry|date=2008-04-17|access-date=2008-06-04|publisher=Las Cruces Sun-News |archive-url = https://web.archive.org/web/20080611144914/http://www.lcsun-news.com/ci_8960289 <!-- Bot retrieved archive --> |archive-date = 2008-06-11}}</ref> |
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==Recreation== |
==Recreation== |
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The Gila River between [[Virden, New Mexico]], and [[Solomon, Arizona]], is navigable during spring snowmelt and after summer and autumn storms. The river passes through many scenic canyons and stretches of Class I to III whitewater. Due to its desert surroundings, the river is characterized by erratic flows and flash floods that reach high peaks and drop off just as quickly. The Gila's Salt River tributary has even more difficult whitewater, ranging up to Class IV in places, and often has higher and more dependable flows than the Gila. |
The Gila River between [[Virden, New Mexico]], and [[Solomon, Arizona]], is navigable during spring snowmelt and after summer and autumn storms. The river passes through many scenic canyons and stretches of Class I to III whitewater. Due to its desert surroundings, the river is characterized by erratic flows and flash floods that reach high peaks and drop off just as quickly. The Gila's Salt River tributary has even more difficult whitewater, ranging up to Class IV in places, and often has higher and more dependable flows than the Gila. |
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Boating and fishing are popular on San Carlos Lake and other basin reservoirs, including [[Lake Pleasant Regional Park|Lake Pleasant]] and [[Theodore Roosevelt Lake]]. The river system has 36 fish species,<ref>Benke and Cushing, p. 531</ref> including [[largemouth bass]], [[Centrarchidae|sunfish]], [[channel catfish]], [[flathead catfish]], and [[Gila trout]] ''(Oncorhynchus gilae gilae)''. |
Boating and fishing are popular on San Carlos Lake and other basin reservoirs, including [[Lake Pleasant Regional Park|Lake Pleasant]] and [[Theodore Roosevelt Lake]]. The river system has 36 fish species,<ref>Benke and Cushing, p. 531</ref> including [[largemouth bass]], [[Centrarchidae|sunfish]], [[channel catfish]], [[flathead catfish]], and [[Gila trout]] ''(Oncorhynchus gilae gilae)''. |
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==Variant names== |
==Variant names== |
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==See also== |
==See also== |
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{{Div col|small=yes}} |
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[[File:GilaRiverAtUS95.jpg|thumb|Gila River at U.S. 95]] |
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*[[ |
*[[Gila and Salt River Meridian]] |
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*[[ |
*[[Gila River War Relocation Center]] |
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*[[List of Arizona rivers]] |
*[[List of Arizona rivers]] |
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*[[List of New Mexico rivers]] |
*[[List of New Mexico rivers]] |
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*[[List of longest rivers of the United States (by main stem)]] |
*[[List of longest rivers of the United States (by main stem)]] |
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*[[Gila River War Relocation Center]] |
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*[[Needle's Eye Wilderness]] |
*[[Needle's Eye Wilderness]] |
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*[[ |
*[[San Francisco River (central Arizona)|San Francisco River]] |
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{{Div col end}} |
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== References == |
== References == |
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=== Citations === |
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===Footnotes=== |
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{{reflist|2}} |
{{reflist|2}} |
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*[https://web.archive.org/web/20080716183043/http://www.azgfd.gov/outdoor_recreation/BoatingLocationsMap.shtml Arizona Boating Locations Facilities Map] |
*[https://web.archive.org/web/20080716183043/http://www.azgfd.gov/outdoor_recreation/BoatingLocationsMap.shtml Arizona Boating Locations Facilities Map] |
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*[https://web.archive.org/web/20100920171711/http://www.azgfd.gov/h_f/FishingLocationsMap.shtml Arizona Fishing Locations Map] |
*[https://web.archive.org/web/20100920171711/http://www.azgfd.gov/h_f/FishingLocationsMap.shtml Arizona Fishing Locations Map] |
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*[http://www.azgfd.gov/h_f/where_fish.shtml Where to Fish in Arizona Species Information] |
*[http://www.azgfd.gov/h_f/where_fish.shtml Where to Fish in Arizona Species Information] {{Webarchive|url=https://web.archive.org/web/20080730094359/http://www.azgfd.gov/h_f/where_fish.shtml |date=2008-07-30 }} |
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*[http://www.azgfd.gov/h_f/edits/lake_levels.shtml Arizona Lake Levels] |
*[http://www.azgfd.gov/h_f/edits/lake_levels.shtml Arizona Lake Levels] {{Webarchive|url=https://web.archive.org/web/20100716011638/http://www.azgfd.gov/h_f/edits/lake_levels.shtml |date=2010-07-16 }} |
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{{Rivers and streams of Arizona}} |
{{Rivers and streams of Arizona}} |
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{{Colorado_River_system}} |
{{Colorado_River_system}} |
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{{authority control}} |
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[[Category:Gila River| |
[[Category:Gila River| ]] |
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[[Category:Arizona placenames of Native American origin]] |
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[[Category:Rivers of Arizona]] |
[[Category:Rivers of Arizona]] |
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[[Category:Rivers of New Mexico]] |
[[Category:Rivers of New Mexico]] |
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[[Category: |
[[Category:Rivers of Pinal County, Arizona]] |
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[[Category:Rivers of Sierra County, New Mexico]] |
[[Category:Rivers of Sierra County, New Mexico]] |
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[[Category:Rivers of Pinal County, Arizona]] |
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[[Category:Sonoran Desert]] |
[[Category:Sonoran Desert]] |
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[[Category:Tributaries of the Lower Colorado River in Arizona]] |
Latest revision as of 03:48, 19 November 2024
Gila River | |
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Location | |
Country | United States |
State | Arizona |
State | New Mexico |
Physical characteristics | |
Source | Confluence of East and West Forks |
• location | Grant County, New Mexico |
• coordinates | 33°10′47″N 108°12′22″W / 33.17972°N 108.20611°W[1] |
• elevation | 5,551 ft (1,692 m) |
Mouth | Colorado River |
• location | Yuma, Arizona |
• coordinates | 32°43′11″N 114°33′19″W / 32.71972°N 114.55528°W[1] |
• elevation | 118 ft (36 m) |
Length | 649 mi (1,044 km)[2] |
Basin size | 58,200 sq mi (151,000 km2)[2] |
Discharge | |
• location | Dome, AZ; 12 mi (19 km) from the mouth[3] |
• average | 247 cu ft/s (7.0 m3/s)[3] |
• minimum | 0 cu ft/s (0 m3/s) |
• maximum | 200,000 cu ft/s (5,700 m3/s) |
Basin features | |
Tributaries | |
• left | San Simon River, San Pedro River, Santa Cruz River |
• right | San Francisco River, Salt River, Agua Fria River, Hassayampa River |
The Gila River (/ˈhiːlə/; O'odham [Pima]: Keli Akimel or simply Akimel, Quechan: Haa Siʼil, Maricopa language: Xiil[4]) is a 649-mile-long (1,044 km)[2] tributary of the Colorado River flowing through New Mexico and Arizona in the United States. The river drains an arid watershed of nearly 60,000 square miles (160,000 km2) that lies mostly within the U.S., but also extends into northern Sonora, Mexico.
Indigenous peoples have lived along the river for at least 2,000 years, establishing complex agricultural societies before European exploration of the region began in the 16th century. European Americans did not permanently settle the Gila River watershed until the mid-19th century.
During the 20th century, development in the Gila River watershed prompted the construction of large diversion and flood control structures on the river and its tributaries, and consequently the Gila contributes only a small fraction of its historic flow to the Colorado.[5] The historic natural discharge of the river was around 1,900 cubic feet per second (54 m3/s), but has declined to only 247 cubic feet per second (7.0 m3/s). The engineering projects transformed much of the river valley and its surroundings from arid desert into irrigated land, and supply water to more than five million people in the Phoenix and Tucson metropolitan areas who live in the watershed.
Geography
[edit]The Gila River has its source in western New Mexico, in Sierra County on the western slopes of the Continental Divide in the Black Range. It flows southwest through the Gila National Forest, the Gila Wilderness, and Gila Cliff Dwellings National Monument, then westward into Arizona, past the town of Safford. After flowing along the southern slope of the Gila Mountains in Graham County through a series of canyons, the Gila is impounded by Coolidge Dam in San Carlos Lake south of Peridot.
It emerges from the mountains into the valley southeast of Phoenix, Arizona, where it crosses the Gila River Indian Reservation as an intermittent stream due to large irrigation diversions, primarily at the Hayden Ashurst Diversion Dam. Well west of Phoenix, the river bends sharply southward along the Gila Bend Mountains, then it swings westward again near the town of Gila Bend. It flows southwestward between the Gila Mountains to the south and the Languna and Muggins ranges to the north in Yuma County, and finally it empties into the Colorado at Yuma, Arizona.
The Gila is joined by many tributaries, beginning with the East and West Forks of the river, which combine to form the main stem near Gila Hot Springs in New Mexico. Above Safford, it is joined by the San Francisco River and the intermittent San Simon River. Further downstream, it is joined by the San Carlos River from the north in San Carlos Lake. At Winkelman, Arizona, it picks up the San Pedro River and then is joined by the Santa Cruz River south of Casa Grande. The Salt River, its main tributary, joins in the Phoenix metropolitan area, and further west the Gila receives its last two major tributaries, the Agua Fria and Hassayampa Rivers, from the north.
Although the Gila River flows entirely within the United States, the headwaters of two tributaries – the San Pedro and Santa Cruz Rivers – extend into Mexico. About 1,630 sq mi (4,200 km2), or 2.8% of the Gila's 58,200-square-mile (151,000 km2) watershed, is in Mexico.[6] A further 3,300 sq mi (8,500 km2) or 5.7% lies within New Mexico, while the remaining majority, 53,270 sq mi (138,000 km2) or 91.5%, is in Arizona.[7]
History
[edit]A band of Pima (autonym "Akimel O'odham", river people), the Keli Akimel O'odham (Gila River People), have lived on the banks of the Gila River since before the arrival of Spanish explorers. Popular theory says that the word "Gila" was derived from a Spanish contraction of Hah-quah-sa-eel, a Yuma word meaning "running water which is salty".[8] Their traditional way of life (himdagĭ, sometimes rendered in English as Him-dak) was and is centered at the river, which is considered holy. Traditionally, sand from the banks of the river is used as an exfoliant when bathing (often in rainstorms, especially during the monsoon). Indigenous peoples such as the Hohokam were responsible for creating large, complex civilizations along the Middle Gila River and Salt River between 600 and 1450 AD. These native civilizations depended largely on irrigated agriculture, for which they constructed over 200 miles (320 km) of canals.[9] The upper Gila was inhabited by the Mogollon culture over most of the same time period, in settlements like those at Gila Cliff Dwellings National Monument in the later period.
The first European to see the Gila River was possibly Spanish explorer and missionary Juan de la Asunción. Asunción reached the Gila in 1538 after traveling northwards along one of its tributaries, either the San Pedro or Santa Cruz.[10] In 1540, Hernando de Alarcón sailed up the Colorado and Gila Rivers; maps drawn by his expedition show the river as the Miraflores or Brazos de la Miraflores.[11]
During the Mexican–American War, General Stephen Watts Kearny marched 100 cavalrymen from the 1st U.S. Dragoons along the Gila River in November 1846.[12] This detachment was guided by Kit Carson. The Mormon Battalion followed Kearny's troops, building a wagon trail roughly following the river from December 1846 to January 1847.[13]
After the Treaty of Guadalupe-Hidalgo in 1848, the Gila River served as a part of the border between the United States and Mexico until the 1853 Gadsden Purchase extended American territory well south of the Gila. The confluence of the Gila with the Colorado River was also used as a reference point for the southern border of California. Beginning in 1871, mainly Mormon settlers populated the Gila River valley around modern Phoenix, using the Gila, Salt, and San Pedro Rivers for irrigation and establishing at least six major settlements.[14]
In 1944, 25 German prisoners of war pulled off the largest and most spectacular escape from an American compound during the war, digging a 178-foot (54 m) tunnel out of the Navy’s Papago Park Prisoner of War Camp in Arizona. All of the men were eventually captured, though some remained at large for more than a month. Among the last to be captured were three German soldiers who had based their audacious but ill-fated escape plans on a stolen highway map of Arizona, which showed the Gila River leading to the Colorado River, which in turn led to Mexico. Devising a scheme to flee by water, the Germans constructed a collapsible kayak under the noses of their American captors, tested it in a makeshift pool within the prison compound, then sneaked it out through the tunnel. Their plan was perfect – except for the map. The Gila, shown as a healthy blue waterway, turned out to be little more than a dry rut.[15]
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The McPhaul Suspension Bridge on a former section of US Route 95 spans the Gila between the Gila and Laguna ranges in Yuma County. The bridge is listed on the National Register of Historic Places.
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The Gila River near Coolidge Dam in Arizona
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This patch of desert south of Buckeye, Arizona, drains east and west from a minor drainage divide. When they flow, both sides flow to the Gila River.
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Painted Rock Dam in central Arizona, with its usually dry reservoir nearly full after heavy runoff in 2005
Hydrology
[edit]The only major dam on the Gila River is Coolidge Dam, 31 miles (50 km) southeast of Globe, Arizona, which forms San Carlos Lake. The Painted Rock Dam crosses the Gila near Gila Bend, although the river is intermittent at that point. The majority of the water is diverted at the Ashurst-Hayden Diversion Dam near Florence, Arizona. A number of minor diversion dams have been built on the river between the Painted Rock Dam and the Coolidge Dam, including the Gillespie Dam, which was breached during a flood in 1993.
Many dams have been built on tributaries to the Gila River, including Theodore Roosevelt Dam, Horse Mesa Dam, and Mormon Flat Dam on the Salt River, New Waddell Dam on the Agua Fria River, and Bartlett Dam on the Verde River.
Many major dams in the Gila River system were built and operated by the U.S. Bureau of Reclamation, which also constructed most of the large dams throughout the Colorado River basin. Others, such as Coolidge Dam, are owned by local water supply agencies, irrigation districts, or Native American tribes.
The Gila River and its main tributary, the Salt River, were both perennial streams carrying large volumes of water – the Gila was once navigable by large riverboats from its mouth to near Phoenix, and by smaller craft from Phoenix nearly to the Arizona-New Mexico border – until irrigation and municipal water diversions turned both into usually dry rivers which carry water only after local downpours create flooding. Below Phoenix to the Colorado River, the Gila is usually either a trickle or completely dry, as is also the lower Salt from Granite Reef Diversion Dam downstream to the Gila, but both rivers can carry large volumes of water following rainfall.
The historic width of the Gila River varied from 150 to 1,200 feet (46 to 366 m) with a depth of 2 to 40 feet (0.61 to 12.19 m). Its natural discharge was roughly 1,300,000 acre-feet (1.6 km3) per year, with a mean flow of about 1,800 cubic feet per second (51 m3/s) at the mouth.[16] The river's modern discharge near the mouth is less than 180,000 acre-feet (0.22 km3) per year, with an average flow of just 247 cubic feet per second (7.0 m3/s).[3] Overdraft from the Gila River system prompted the construction of the Central Arizona Project, which delivers some 1,500,000 acre-feet (1.9 km3) annually from the Colorado River to supplement water supplies in the basin.[17]
The upper Gila River, including its entire length within New Mexico, is a free-flowing one. Recent efforts to allow for damming or otherwise diverting this stretch have met with stiff political resistance, having been named as one of the nation's most endangered rivers due to proposed dam projects such as Hooker Dam. During his time in office, former New Mexico Governor Bill Richardson had promised to block any such attempt during his term, and he had even considered pushing for a statutory prohibition against any such projects on the state's portion of the river.[18]
Recreation
[edit]The Gila River between Virden, New Mexico, and Solomon, Arizona, is navigable during spring snowmelt and after summer and autumn storms. The river passes through many scenic canyons and stretches of Class I to III whitewater. Due to its desert surroundings, the river is characterized by erratic flows and flash floods that reach high peaks and drop off just as quickly. The Gila's Salt River tributary has even more difficult whitewater, ranging up to Class IV in places, and often has higher and more dependable flows than the Gila.
Boating and fishing are popular on San Carlos Lake and other basin reservoirs, including Lake Pleasant and Theodore Roosevelt Lake. The river system has 36 fish species,[19] including largemouth bass, sunfish, channel catfish, flathead catfish, and Gila trout (Oncorhynchus gilae gilae).
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Middle Fork of the Gila River, SW New Mexico
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Rock spires above the East Fork of the Gila River, Gila Wilderness
Variant names
[edit]The Gila River has also been known as:[1]
- Akee-mull
- Apache de Gila
- Brazo de Miraflores
- Cina`ahuwipi (Chemehuevi language)
- Hah-quah-sa eel (Yuma language)
- Hela River
- Jila River
- Rio Azul
- Rio Gila
- Rio de las Balsas
- Rio del Nombre Jesus
- Rio del los Apostoles
- Zila River
- Xila River
- Keli Akimel
See also
[edit]References
[edit]Citations
[edit]- ^ a b c "Gila River". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. 1980-02-08. Retrieved 2012-03-16.
- ^ a b c Kammerer, J.C. "Largest Rivers in the United States". U.S. Geological Survey. Retrieved 2012-03-16.
- ^ a b c "USGS Gage #09520500 on the Gila River near Dome, AZ" (PDF). National Water Information System. U.S. Geological Survey. 1903–2011. Retrieved 2012-03-16.
- ^ Antone, Caroline. Piipayk m'iim. Salt River: Oʼodham Piipaash Language Program, 2000.
- ^ "The Gila is mostly bone dry in its lower reaches" (Jonathan Waterman, "American Nile: Saving the Colorado", National Geographic).
- ^ "Boundary Descriptions and Names of Regions, Subregions, Accounting Units and Cataloging Units". U.S. Geological Survey. Retrieved 2012-03-16.
- ^ "USGS Gage #09432000 on the Gila River Below Blue Creek, Near Virden, NM" (PDF). National Water Information System. U.S. Geological Survey. 1914–2011. Archived from the original (PDF) on 2013-07-20. Retrieved 2012-03-16.
- ^ "Gila National Forest (archived)". United States Forest Service. 2003-12-04. Archived from the original on January 11, 2006. Retrieved 2007-10-16.
- ^ Howard, Jerry B. "Hohokam Legacy: Desert Canals". Pueblo Grande Museum Profiles No. 12. WaterHistory.org. Archived from the original on 2012-01-24. Retrieved 2012-03-16.
- ^ Hartmann, William K.; Hartmann, Gayle Harrison (1972). "Juan de la Asunción, 1538: First Spanish Explorer of Arizona?". Kiva. 37 (2): 93–103. doi:10.1080/00231940.1972.11757756.
- ^ "Rivers and Mountains". Books of the Southwest. University of Arizona. Archived from the original on 2010-07-09. Retrieved 2012-03-16.
- ^ Turner, Henry Smith (1966). The original journals of Henry Smith Turner with Stephen Watts Kearny to New Mexico and California, 1846–1847. Edited and with an introd. by Dwight L. Clarke. Norman: University of Oklahoma Press. p. 87.
- ^ Tyler, Daniel (1969). A Concise History of the Mormon Battalion in the Mexican War, 1846–1847. Glorieta, NM: Rio Grande Press. p. 233. ISBN 978-0873800112.
- ^ Peterson, Charles S. (1992). "Pioneer Settlements in Arizona". Light Planet. Archived from the original on 2012-02-20. Retrieved 2012-03-16.
- ^ Harvey, Miles, 2000, The Island of Lost Maps. p. 154.[ISBN missing]
- ^ Cohen, Michael J.; Henges-Jeck, Christine; Castillo-Moreno, Gerardo (2001). "A preliminary water balance for the Colorado River delta, 1992–1998" (PDF). Journal of Arid Environments. 49 (1): 35–48. Bibcode:2001JArEn..49...35C. doi:10.1006/jare.2001.0834.
- ^ "Biological Opinion on the Transportation and Delivery of Central Arizona Project Water to the Gila River Basin in Arizona and New Mexico". Native Aquatic Species of the Gila River Basin in Arizona and New Mexico. U.S. Bureau of Reclamation. 2010-08-30. Retrieved 2012-03-18.
- ^ Massey, Barry (2008-04-17). "NM governor pledges to fight Gila River diversion". Las Cruces Sun-News. Archived from the original on 2008-06-11. Retrieved 2008-06-04.
- ^ Benke and Cushing, p. 531
Works cited
[edit]- Benke, Arthur C.; Cushing, Colbert E. (2005). Rivers of North America. Academic Press. ISBN 978-0-12088-253-3.