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{{short description|River in Colorado and Nebraska, United States}} {{Use American English|date=February 2025}} {{more citations needed|date=January 2011}} {{Infobox river | name = South Platte River<ref name=gnis>{{cite gnis|id= 201759|name=South Platte River|access-date=January 5, 2025}}</ref> | native_name ={{native name|lkt|Wašíŋ Wakpá}} | image = Sprco2.jpg | image_alt = | image_caption = South Platte River in [[Douglas County, Colorado|Douglas County]], [[Colorado]] | map = South Platte basin map.png | map_alt = South Platte River watershed | map_caption = | mapframe = yes | mapframe-zoom = 5 | source1_location = Confluence of South Fork and Middle Fork | source1_coordinates= {{coord|39|00|40|N|105|44|25|W}} | mouth_location = Confluence with [[North Platte River]] | mouth_coordinates = {{coord|41|06|50|N|100|40|33|W|display=inline,title}} | progression = [[Platte River|Platte]]—[[Missouri River|Missouri]]—[[Mississippi River|Mississippi]] | length = {{convert|439|mi|km|abbr=on}}<ref name=NHD>U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. [http://viewer.nationalmap.gov/viewer/ The National Map], accessed March 25, 2011</ref> | source1_elevation = | mouth_elevation = {{convert|2762|ft|m|abbr=on}} | discharge1_avg = {{convert|174|ft3/s|abbr=on}} | custom_label = Discharge range | custom_data = {{convert|0|to|4640|ft3/s|abbr=on}}<ref name="wdr">[http://pubs.usgs.gov/wdr/wdr-co-03-1/vol1/pdf/WDR_CO-03-1.pdf Water Data Report, Colorado 2003], from [http://pubs.usgs.gov/wdr/wdr-co-03-1/ Water Resources Data Colorado Water Year 2003], [[United States Geological Survey|USGS]].</ref> | extra = }} [[File:S.PlatteBridge.jpg|thumb|The South Platte River in [[Platte Canyon]], Colorado]] [[File:South Platter River Denver 2017.jpg|thumb|South Platte River in [[Denver, Colorado]]]] [[File:South Platte River kayaking Eleven Mile Canyon.jpg|thumb|Kayakers in Eleven Mile Canyon]] The '''South Platte River''' is one of the two principal [[tributaries]] of the [[Platte River]]. Flowing through the [[U.S. state]]s of [[Colorado]] and [[Nebraska]], it is itself a major river of the American [[Midwestern United States|Midwest]] and the American [[Southwestern United States|Southwest]]/[[Mountain States|Mountain West]]. Its [[drainage basin]] includes much of the eastern flank of the [[Rocky Mountains]] in Colorado, much of the populated region known as the [[Colorado Front Range]] and [[Colorado Eastern Plains|Eastern Plains]], and a portion of southeastern [[Wyoming]] in the vicinity of the city of [[Cheyenne, Wyoming|Cheyenne]]. It joins the [[North Platte River]] in western Nebraska to form the Platte, which then flows across Nebraska to the [[Missouri River|Missouri]]. The river serves as the principal source of water for eastern Colorado. In its valley along the foothills in Colorado, it has permitted [[agriculture]] in an area of the [[Colorado Piedmont]] and [[Great Plains]] that is otherwise arid. ==Description== The river is formed in [[Park County, Colorado]], southwest of [[Denver, Colorado|Denver]] in the [[South Park (Park County, Colorado)|South Park]] grassland basin by the confluence of the [[South Fork South Platte River|South Fork]] and [[Middle Fork South Platte River|Middle Fork]], about {{convert|15|mi|km|abbr=on}} southeast of [[Fairplay, Colorado|Fairplay]]. Both forks rise along the eastern flank of the [[Mosquito Range]], on the western side of South Park, which is drained by the tributaries at the headwaters of the river. From South Park, it passes through {{convert|50|mi|km|abbr=on}} of the [[Platte Canyon]] and its lower section, Waterton Canyon. Here, it is joined by the [[North Fork South Platte River|North Fork]] before emerging from the foothills southwest of the Denver suburb of [[Littleton, Colorado|Littleton]]. At Littleton, the river is impounded to form [[Chatfield Reservoir]], a flood-control basin for the [[Denver metropolitan area]]. The river flows north through central Denver, which was founded along its banks at its confluence with [[Cherry Creek (Colorado)|Cherry Creek]]. The valley through Denver is highly industrialized, serving generally as the route for both the [[railway|railroad]] lines, as well as [[Interstate 25]]. On the north side of Denver, it is joined somewhat inconspicuously by [[Clear Creek (Colorado)|Clear Creek]], which descends from the mountains to the west in a canyon that was the cradle of the [[Pike's Peak Gold Rush]]. North of Denver, it flows through the agricultural heartland of the Piedmont (a [[shale]] region that was formed through erosion by the ancestor of the river following the creation of the Rockies). It flows directly past the communities of [[Brighton, Colorado|Brighton]] and [[Fort Lupton, Colorado|Fort Lupton]], and is joined in succession by [[Saint Vrain Creek]], the [[Little Thompson River]], the [[Big Thompson River]], and the [[Cache la Poudre River]], which it receives just east of [[Greeley, Colorado|Greeley]]. East of Greeley, it turns eastward, flowing across the [[Colorado Eastern Plains]], past [[Fort Morgan, Colorado|Fort Morgan]] and [[Brush, Colorado|Brush]], where it turns northeastward. It continues past [[Sterling, Colorado|Sterling]], and runs into Nebraska between [[Julesburg, Colorado]], and [[Big Springs, Nebraska]]. In Nebraska, it passes south of [[Ogallala, Nebraska|Ogallala]] and joins the [[North Platte River]] near the city of [[North Platte, Nebraska|North Platte]]. The South Platte River through Denver is on the U.S. [[Environmental Protection Agency]]'s (US EPA) list of impaired waterbodies for pathogen impairment, with ''E. coli ''as the representative pathogen species. Other water issues involve the appearance of the [[New Zealand mud snail]] and [[zebra mussel]]. The flows of the South Platte have been greatly modified by human activity. Originally the river was seasonal north of Fort Morgan to its confluence with the North Platte. In the 1800s the river would disappear in July, August, and September due to low flows and a sandy river bottom. By 1910 the increase in agriculture caused the river to reach the border of Colorado and Wyoming due to [[return flow]]s and dams holding back water later in the year. Increasing diversions from the upper [[Colorado River]] in the 20th century mean that flows reach the North Platte year round.<ref>{{cite book |last1=Committee on Western Water Management |title=Water Transfers in the West: Efficiency, Equity, and the Environment |date=1992 |publisher=National Academy Press |location=Washington, D.C. |isbn=978-0-309-04528-5 |pages=140–142 |url=https://archive.org/details/watertransfersin0000unse/page/140 |access-date=28 May 2024}}</ref> ==History== The South Platte was originally called Niinéniiniicíihéhe by the native Arapaho people who lived on its banks. The early Spanish explorers called it the Rio Chato (calm river). In 1702, it was named the Rio Jesus Maria by Captain Jose Naranjo, the Indigenous-Spanish scout and captain of war of the New Mexico Indian Auxiliaries, who was ordered by the viceroy of New Spain to search the Tierra Incognita for a French incursion into New Mexico.<ref>''Nebraska: A Guide to the Cornhusker State.'' [[Nebraska State Historical Society]]. p. 46.</ref> The South Platte also served as a vital water source in Colorado. Long before the city of Denver was created, many travelers came to the South Platte River to escape the arid Great Plains. These people could survive the heat, but not without the vital water source that the South Platte gave them. Buckets and wells sufficed as a water system for a while, but eventually, the Denver Water System was created.<ref>[http://www.denverwater.org/AboutUs/History/ Denver Water History] {{webarchive|url=https://web.archive.org/web/20160903063933/http://www.denverwater.org/AboutUs/History/ |date=2016-09-03 }}. Accessed June 23, 2014.</ref> In the late 1830s, four [[Fur trade|fur trading]] outposts were established on the river.<ref>{{Cite journal |last=Hafen |first=L. R. |date=1925 |title=The Early Fur Trade Posts on the South Platte |url=https://www.jstor.org/stable/1889565 |journal=The Mississippi Valley Historical Review |volume=12 |issue=3 |pages=334–341 |doi=10.2307/1889565 |issn=0161-391X}}</ref> ==Dams== In an arid region of the United States, the South Platte is marked with several dams. The first notable water impoundment on the South Platte is [[Antero Reservoir]]. "Antero" is derived from the Spanish word "delantero", which means "foremost" or "head", as the reservoir was the first dam on the South Platte River near the river's origin. The next dam is Spinney Mountain Reservoir. At capacity, Spinney Mountain covers {{convert|2500|acre|km2}}. A bottom-release dam, Spinney releases to the east of the inlet. Two miles below Spinney Mountain Reservoir, the river enters Eleven Mile Reservoir, with a capacity of {{convert|97000|acre.ft|m3|lk=in}}. The Eleven Mile Reservoir Dam drains into Eleven Mile Canyon, which runs through [[United States Forest Service|Forest Service]] land. Three former Colorado towns, Howbert, Idlewild, and Freshwater Station, were submerged under the reservoir when it was built.<ref>Laura King Van Dusen, "Forty-Six Years in Howbert: 1887-1933: Former Ranching, Railroading Community Covered by Eleven-Mile Reservoir", ''Historic Tales from Park County: Parked in the Past'' ([[Charleston, South Carolina|Charleston]], [[South Carolina]]: The History Press, 2013), {{ISBN|978-1-62619-161-7}}, pp. 97–104.</ref> From [[Eleven Mile Canyon]], the South Platte runs northeast to [[Cheesman Reservoir]], named for Denver water pioneer [[Walter Cheesman|Walter S. Cheesman]]. At its completion in 1905, the dam was the world's tallest gravity dam, at {{convert|221|ft|m|abbr=on}} above the streambed. The reservoir and related facilities were purchased in November 1918 by the Denver Water Board. Cheesman was the first reservoir of Denver's mountain storage facilities, and has been designated a National Historic Civil Engineering Landmark. Cheesman Reservoir feeds Cheesman Canyon. Six miles below Cheesman Reservoir is the town of Deckers; there, the river bends north for about {{convert|17|mi|km|abbr=on}} to the confluence with the North Fork of the South Platte. In the late 1980s, a proposal was put forth for the Two Forks Dam, which would have created a reservoir flooding the entire section from the North Fork confluence to the town of Deckers. In 1990, the US EPA vetoed the permit, calling the project an "environmental catastrophe." From the confluence, the river flows towards Denver and enters Strontia Springs Reservoir. Below Strontia Springs, the South Platte runs through [[Waterton Canyon]] before entering Chatfield Reservoir. Chatfield marks the seventh and final dam on the South Platte until it merges with the North Platte. ==Fly fishing overview== The South Platte River is a gold medal western trout river on the eastern slope of Colorado, meaning it produces at least 12 trout of greater than 14 inches in length or greater per acre in areas accessible to the public. The river is well known for its wild trophy population of [[brown trout|brown]] and [[rainbow trout]].<ref>{{cite web |title=Colorado Gold Waters |url=https://coloradogoldmedalwater.tu.org/gold-medal-waters/ |website=Colorado Gold Medal Waters |publisher=Trout Unlimited |access-date=28 May 2024 |language=en}}</ref> As a result of its close proximity to [[Denver]], the river has thousands of [[fly fishing]] enthusiasts visit each year. With seven dams on the river, the South Platte is considered a [[tailwater]] fishery. Most of these dams are bottom released, which allows for both stable water temperatures and year-round fly fishing. Popular fly-fishing stretches of the river include [[Waterton Canyon]], [[Cheesman Canyon]], and the Dream Stream. ==See also== *[[List of rivers of Colorado]] *[[List of rivers of Nebraska]] *[[South Platte River Trail Scenic and Historic Byway]], a 19-mile byway in Sedgwick County, Colorado *[[South Platte Trail]], the historic trail along the South Platte River, from northwestern Colorado to the Denver area == References == {{reflist}} ==External links== {{Commons category}} *[https://web.archive.org/web/20130114024606/http://www.denverwater.org/Recreation/Antero/ Antero Reservoir] *[http://parks.state.co.us/parks/chatfield/ Chatfield Reservoir] *[https://web.archive.org/web/20130106114515/http://www.denverwater.org/Recreation/Cheesman/ Cheesman Reservoir] *[http://co.water.usgs.gov/nawqa/splt/ USGS: South Platte River Basin] *[https://web.archive.org/web/20081011013504/http://sciencepolicy.colorado.edu/wwa/archives/gis/hydro_data/platt.html University of Colorado: GIS Hydro Data for the South Platte] *[https://web.archive.org/web/20120307091057/http://www.denvergov.org/EAP/WaterQualityProgram/MayorsWaterQualityInitiative/tabid/424856/Default.aspx City of Denver: South Platte Initiative] *[https://web.archive.org/web/20100125110835/http://parks.state.co.us/parks/elevenmile Eleven Mile Reservoir] *[http://www.greenwayfoundation.org The Greenway Foundation] *[http://parks.state.co.us/Parks/SpinneyMountain Spinney Mountain Reservoir] *[https://web.archive.org/web/20130103092611/http://www.denverwater.org/recreation/watertoncanyon/ Strontia Springs Reservoir and Waterton Canyon] {{authority control}} [[Category:Rivers of Colorado]] [[Category:Rivers of Nebraska]] [[Category:Rivers of Park County, Colorado]] [[Category:Rivers of Deuel County, Nebraska]] [[Category:Rivers of Keith County, Nebraska]] [[Category:Tributaries of the Platte River]] [[Category:Rivers of Sedgwick County, Colorado]] [[Category:Rivers of Douglas County, Colorado]] [[Category:Rivers of Jefferson County, Colorado]] [[Category:Rivers of Weld County, Colorado]] [[Category:Rivers of Morgan County, Colorado]] [[Category:Rivers of Logan County, Colorado]]
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