Skip to content
Surf Wiki
Save to docs
general/rivers-of-washington-state

From Surf Wiki (app.surf) — the open knowledge base

Colville River (Washington)


FieldValue
nameColville River
name_etymology
pushpin_map_caption
subdivision_type1Country
subdivision_name1United States
subdivision_type2State
subdivision_name2Washington
subdivision_name5
discharge1_locationmouth
discharge1_avg429 cuft/s
discharge1_max
source1_coordinates
source1_elevation2146 ft
mouthColumbia River
mouth_locationFranklin D. Roosevelt Lake, Washington (state)
mouth_coordinates
mouth_elevation1300 ft
basin_size_mi21010
basin_size_ref

The Colville River is a 60-mile (100 km) long tributary of the Columbia River in northeastern Washington in the United States. The Colville River begins in southern Stevens County, Washington at the confluence of Sheep Creek and Deer Creek. It flows northwest past Colville and into the Columbia River near Kettle Falls.

Watershed

History and Culture

In the beginning, the Colville River was a place of abundance. The path of the Colville River was carved by Ice Age glaciers. Mile high ice sheets coming from Canada flowed over many mountain peaks near the Colville River, leading to rounded mountain tops at lower elevations.  Around 10,000 years ago the glacial ice melted, opening the way for settlement near the river. Native Americans came first around 9,000 years ago. At this time there were salmon in the river bringing Native Americans near the Colville River yearly for a first salmon ceremony. It is estimated that Native Americans caught more than 1,000 salmon a day at Kettle Falls during peak runs. By 1826, fur trappers, mostly catching beavers, moved into Fort Colville.

Pollution

The Colville River has two main point sources of pollution. They include two water waste treatment plants (WWTP): the city of Colville and the city of Chewelah. Ammonia, a toxic substance for aquatic life, has concentrations highest downstream the Chewelah and Colville WWTP discharges. In fact, modeled concentrations at the Colville WWTP mixing zone predict concentrations of ammonia and chlorine above acute water quality standards. Besides toxicity, ammonia also is a concern for dissolved oxygen content within the water. It has been demonstrated that dissolved oxygen concentrations decrease suddenly downstream from the Chewelah and Colville WWTPs in summer months. One explanation is that the excess ammonia is taken up by algae causing a decrease in dissolved oxygen content, which may harm aquatic life. The risk of these effects is greatest August through October, deemed as the critical period for the Colville River when possible physical, chemical, and biological adverse effects of a pollutant are maximized.

Current Projects

The United States Geological Survey is currently working with the Stevens County Conservation District to create a watershed plan. This plan will address water quality, quantity, and in-stream flows pertaining to the Colville River. In addition, The Lands Council from Spokane, Washington is working to relocate beavers to the Colville National Forest. Beavers are known to slow streams, create dams and lodges for improved habitats for other animals and insects, gather silt, store and cool water. The Land Council hopes these beavers will aid the Colville River's ecosystem along with other water bodies downstream.

References

References

  1. {{Gnis. 1517986. Colville River, [[USGS]] GNIS
  2. [[Google Earth]] elevation for [[GNIS]] source coordinates.
  3. [[Google Earth]] elevation for [[GNIS]] mouth coordinates.
  4. [https://www.nwcouncil.org/sites/default/files/29_uprcol_overview.pdf Upper Columbia Subbasin Overview], Northwest Power and Conservation Council
  5. Murray, Dennis; Pelletier (March 2003). "Colville River Dissolved Oxygen Total Maximum Daily Load" (PDF). ''Washington State Department of Ecology'': 1–49.
  6. Pelletier, Gregory (January 1997). "Pollutant Loading Capacity and Recommendations for Total Maximum Daily Loads" (PDF). ''Washington State Department of Ecology'': 1–136.
  7. "[https://www.usgs.gov/centers/washington-water-science-center/science/colville-river-basin Colville River Basin. U.S. Geological Survey]". ''www.usgs.gov''. Retrieved 2023-11-08.
  8. Francovich, Eli (September 18, 2019). "Beavers in Washington: a 'sizzling hotbed of castor relocation'". ''The Spokesman-Review''. Retrieved November 16, 2023.
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

Want to explore this topic further?

Ask Mako anything about Colville River (Washington) — get instant answers, deeper analysis, and related topics.

Research with Mako

Free with your Surf account

Content sourced from Wikipedia, available under CC BY-SA 4.0.

This content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.

Report