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The Spokane River is a tributary of the Columbia River, approximately Template:Convert long, in northern Idaho and eastern Washington in the United States. It drains a low mountainous area east of the Columbia, passing through the Spokane Valley and the city of Spokane, Washington.

DescriptionEdit

The Spokane River drains the northern part of Lake Coeur d'Alene in the Idaho Panhandle, emptying into the Columbia River at Franklin D. Roosevelt Lake, approximately Template:Convert downstream.<ref name="NRC-92">National Research Council, 2005: p. 92</ref><ref>Soltero et al., 1994: p. 460</ref>

From Lake Coeur d'Alene, the Spokane River traverses the Rathdrum Prairie until reaching Post Falls, Idaho where it passes over a Post Falls Dam, and a natural 40-foot waterfall. Continuing westward it passes over 6 more dams, three of which (Upriver Dam, Upper Falls Dam, Monroe Street Dam) are located in the city of Spokane.<ref name="NRC-92" /> In Spokane, it flows over the Spokane Falls, which are located in the heart of Downtown Spokane,<ref name="NRC-92" /> approximately one third of the way down the river's length.<ref name="Ruby-8">Template:Cite book</ref> About a mile later,Template:Citation needed the river receives Latah Creek from the southeast.<ref name="Ruby-8" /> Soon afterwards, it is met from the northeast<ref name="Ruby-8" /> by the Little Spokane River, on the western edge of the city of Spokane.<ref name="NRC-92" /> It flows in a zigzag course along the southern edge of the Selkirk Mountains, forming the southern boundary of the Spokane Indian Reservation, where it is impounded by the Long Lake Dam to form Long Lake, a Template:Convert reservoir. It joins Franklin D. Roosevelt Lake on the Columbia from the east at Miles. The site of historic Fort Spokane is located at the confluence of the Spokane and Columbia rivers.<ref>National Park Service. Fort Spokane</ref>

The Spokane River's entire drainage basin is about Template:Convert large, of which Template:Convert are above Post Falls Dam at the outlet of Coeur d'Alene Lake.<ref>Spokane Subbasin Plan Template:Webarchive, Northwest Power and Conservation Council; and Intermountain Subbasin Plan, Coeur d'Alene Template:Webarchive, Northwest Power and Conservation Council</ref> Its mean annual discharge is Template:Convert.<ref name="Benke" />

Human useEdit

Until the 18th century, the Coeur d'Alene (Schḭtsu'umsh) and Spokane Native Americans (along with other Salish peoples) used to live and travel along the banks of the Spokane River.<ref>Template:Cite book</ref><ref>Template:Cite book</ref> In 1807, David Thompson was the first European to cross the Rocky Mountains and explore the area.

Today, the Spokane metropolitan area (population 573,493) is the largest human settlement on the banks of the Spokane River. The metropolitan area of Coeur d'Alene (pop. 170,628) is immediately to the east and upstream of the Spokane metropolitan area. The Spokane River and Lake Coeur d'Alene are the primary sources of recharge for the Spokane Valley–Rathdrum Prairie Aquifer, which is the primary source of drinking water for each of these settlements.<ref name="NRC-93">National Research Council, 2005: p. 93</ref>

PollutionEdit

The Spokane River contains some of the highest concentrations of heavy metals of any river in the state, resulting from pollution coming from Lake Coeur D'Alene and traveling from the Bunker Hill Mine and Smelting Complex Superfund site.<ref>Template:Cite book</ref><ref>Rosen, J.F., Science of the Total Environment, Volume: 303 Issue: 1-2, Pages: 15–23, Published: February 15, 2003</ref>

Spokane's sewage treatment facilities empty their outflow into the Spokane River. In 1889, Spokane built a sewage system that dumped raw sewage directly into the river, which was visibly noticeable by 1920. In 1957 a primary treatment facility was installed; however, this was soon deemed inadequate by the Washington State Department of Ecology. This led to the construction of a more advanced treatment plant that utilized chemical precipitation technology, which was connected in 1975, and operational by 1977.<ref>Template:Cite book</ref>

Fish habitatEdit

File:Long Lake Dam 1.JPG
Long Lake Dam on the Spokane River, the construction of which wiped out the salmon populations that used to travel upstream.

After the Northern Pacific Railway lines arrived in Spokane in 1882, there was rapid growth in milling operations along the river. Many of these mills required dams to provide power for their machinery. As a result of the dams blocking the river, salmon populations in the Spokane plummeted, leading to complaints from many of the people living upstream.<ref>Template:Cite book</ref> After the construction of Little Falls Dam in 1910 by Washington Water Power blocked upstream passage, the river's salmon populations disappeared completely.<ref name="Fahey">Fahey, John (1991); "Power Plays: The Enigma of Little Falls," Pacific Northwest Quarterly 82, no.4 (October 1991), 122–131.</ref>

Steelhead were also abundant on the Spokane River, prior to pollution and the construction of the dams. Today, the Spokane River system is one of the two largest unoccupied stretches of steelhead habitat within their former range.<ref>Template:Cite book</ref>

Today, the Spokane River supports populations of rainbow trout, northern pikeminnow, and Bridgelip Suckers (Catostomus columbianus), as well as several non-native species.<ref name="Fahey" /> Many of the remaining fish, however, are not suitable for human consumption due to the chemical pollution in the river, with signs alongside the river warning that the fish are contaminated with PCBs.<ref>Template:Cite book</ref>

CrossingsEdit

File:Spokane aerial.jpg
Aerial view the Spokane River at Spokane, with Lake Coeur d'Alene in the background

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See alsoEdit

ReferencesEdit

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