Columbia River
| Columbia River | |
|---|---|
Columbia River from Rowena Crest with Interstate 84 on the right | |
Columbia River drainage basin | |
| Etymology | Captain Robert Gray's ship, Columbia Rediviva |
| Nickname(s) | Big River, the River of the West, River Oregon |
| Native name | |
| Location | |
| Country | Canada, United States |
| Province | British Columbia |
| State | Washington, Oregon |
| Cities | Revelstoke, BC, Castlegar, BC, Trail, BC, Wenatchee, WA, East Wenatchee, WA, Tri-Cities, WA, The Dalles, OR, Hood River, OR, Portland, OR, Vancouver, WA, Longview, WA, Astoria, OR |
| Physical characteristics | |
| Source | Columbia Lake |
| • location | British Columbia, Canada |
| • coordinates | 50°13′35″N 115°51′05″W / 50.22639°N 115.85139°W |
| • elevation | 2,690 ft (820 m) |
| Mouth | Pacific Ocean, at Clatsop County, Oregon / Pacific County, Washington |
• coordinates | 46°14′39″N 124°3′29″W / 46.24417°N 124.05806°W |
• elevation | 0 ft (0 m) |
| Length | 1,243 mi (2,000 km) |
| Basin size | 258,000 sq mi (670,000 km2) |
| Discharge | |
| • location | Astoria (near mouth) |
| • average | (Period: 1951–1980)265,000 cu ft/s (7,500 m3/s) (Period: 1969–2023)234,700 cu ft/s (6,650 m3/s) |
| Discharge | |
| • location | Port Westward |
| • average | (Period: 1969–2023)233,700 cu ft/s (6,620 m3/s) |
| • minimum | 63,600 cu ft/s (1,800 m3/s)(Year: 2001) |
| • maximum | 864,000 cu ft/s (24,500 m3/s)(Year: 1996) |
| Discharge | |
| • location | The Dalles |
| • average | (Period: 1879–2023)188,500 cu ft/s (5,340 m3/s) |
| • minimum | 12,100 cu ft/s (340 m3/s)(Year: 1968) |
| • maximum | 1,240,000 cu ft/s (35,000 m3/s)(Year: 1894) |
| Discharge | |
| • location | Priest Rapids Dam |
| • average | (1960–2023)118,200 cu ft/s (3,350 m3/s) |
| • minimum | 36,400 cu ft/s (1,030 m3/s)(Year: 1962) |
| • maximum | 533,000 cu ft/s (15,100 m3/s)(Year: 1961) |
| Discharge | |
| • location | United States and Canada international boundary |
| • average | (Period: 1938– 2023)99,300 cu ft/s (2,810 m3/s) |
| • minimum | 21,200 cu ft/s (600 m3/s)(Year: 1944) |
| • maximum | 550,000 cu ft/s (16,000 m3/s)(Year: 1948) |
| Basin features | |
| Progression | Pacific Ocean |
| River system | Columbia River |
| Tributaries | |
| • left | Spillimacheen River, Beaver River, Illecillewaet River, Incomappleux River, Kootenay River, Pend Oreille River, Spokane River, Crab Creek, Snake River, John Day River, Deschutes River, Willamette River |
| • right | Kicking Horse River, Blaeberry River, Canoe River, Kettle River, Sanpoil River, Okanogan River, Entiat River, Wenatchee River, Yakima River, Lewis River, Cowlitz River |
The Columbia River (Upper Chinook: Wimahl or Wimal; Sahaptin: Nch’i-Wàna or Nchi wana; Sinixt dialect swah'netk'qhu) is the largest river in the Pacific Northwest region of North America. The river forms in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the U.S. state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is 1,243 mi (2,000 km) long, and its largest tributary is the Snake River. Its drainage basin is roughly the size of France and extends into seven states of the United States and one Canadian province. The fourth-largest river in the United States by flow, the Columbia has the greatest flow of any river into the eastern Pacific.
The Columbia and its tributaries have been central to the region's culture and economy for thousands of years. They have been used for transportation since ancient times, linking the region's many cultural groups. The river system hosts many species of anadromous fish, which migrate between freshwater habitats and the saline waters of the Pacific Ocean. These fish—especially the salmon species—provided the core subsistence for native peoples.
The first documented European discovery of the Columbia River occurred when Spanish explorer Bruno de Heceta sighted the river's mouth in 1775. On May 11, 1792, a private American ship, Columbia Rediviva, under Captain Robert Gray from Boston became the first non-indigenous vessel to enter the river. Later in 1792, William Robert Broughton of the British Royal Navy commanding HMS Chatham as part of the Vancouver Expedition, navigated past the Oregon Coast Range and 100 miles (160 km) upriver to what is now Vancouver, Washington. In the following decades, fur-trading companies used the Columbia as a key transportation route. Overland explorers entered the Willamette Valley through the scenic, but treacherous Columbia River Gorge, and pioneers began to settle the valley in increasing numbers. Steamships along the river linked communities and facilitated trade; the arrival of railroads in the late 19th century, many running along the river, supplemented these links.
Since the late 19th century, public and private sectors have extensively developed the river. To aid ship and barge navigation, locks have been built along the lower Columbia and its tributaries, and dredging has opened, maintained, and enlarged shipping channels. Since the early 20th century, dams have been built across the river for power generation, navigation, irrigation, and flood control. The 14 hydroelectric dams on the Columbia's main stem and many more on its tributaries produce more than 44 percent of total U.S. hydroelectric generation. Production of nuclear power has taken place at two sites along the river. Plutonium for nuclear weapons was produced for decades at the Hanford Site, which is now the most contaminated nuclear site in the United States. These developments have greatly altered river environments in the watershed, mainly through industrial pollution and barriers to fish migration.