The Marble Canyon Dam , also known as the Redwall Dam , was a proposed dam on the Colorado River in Arizona , United States. The dam was intended to impound a relatively small reservoir in the central portion of Marble Canyon to develop hydroelectric power. Plans centered on two sites between miles 30 and 40 in the canyon. At one point a 38-mile (61 km) tunnel was proposed to a site just outside Grand Canyon National Park to develop the site's full power generation potential, reducing the Colorado River to a trickle through the park.
148-684: Although first proposed in the 1920s to generate hydroelectricity , work did not begin until the dam was incorporated as part of the U.S. Bureau of Reclamation (USBR)'s Pacific Southwest Water Plan in the 1940s for its Central Arizona component . Together with Bridge Canyon Dam , located at the lower end of the Grand Canyon, it would have provided the hydroelectric power necessary to lift Colorado River water from Lake Havasu to central Arizona's farms and cities, including Phoenix and Tucson . The two dams would have operated as "cash register" facilities to provide funds for future reclamation projects through
296-737: A greenhouse gas . According to the World Commission on Dams report, where the reservoir is large compared to the generating capacity (less than 100 watts per square metre of surface area) and no clearing of the forests in the area was undertaken prior to impoundment of the reservoir, greenhouse gas emissions from the reservoir may be higher than those of a conventional oil-fired thermal generation plant. In boreal reservoirs of Canada and Northern Europe, however, greenhouse gas emissions are typically only 2% to 8% of any kind of conventional fossil-fuel thermal generation. A new class of underwater logging operation that targets drowned forests can mitigate
444-463: A low-head hydro power plant with hydrostatic head of few meters to few tens of meters can be classified either as an SHP or an LHP. The other distinction between SHP and LHP is the degree of the water flow regulation: a typical SHP primarily uses the natural water discharge with very little regulation in comparison to an LHP. Therefore, the term SHP is frequently used as a synonym for the run-of-the-river power plant . The largest power producers in
592-436: A "scenic trickle" – for wildlife and recreational purposes in the Grand Canyon. This water would be released through a 22 megawatt power station at the base of the dam, with an annual energy production of 164 million kilowatt hours. Together, the two dams would utilize most of the 1,900-foot (580 m) elevation drop between Lee's Ferry and Lake Mead , which represents one of the biggest untapped hydroelectric potentials in
740-623: A boundary along the Columbia River, the Oregon Treaty of 1846 set the boundary at the 49th parallel. As part of the treaty, the British retained all areas north of the line while the United States acquired the south. The Columbia River became much of the border between the U.S. territories of Oregon and Washington . Oregon became a U.S. state in 1859, while Washington later entered into
888-564: A complex network of dry canyon-like channels, or coulees that are often braided and sharply gouged into the basalt rock underlying the region's deep topsoil. Numerous flat-topped buttes with rich soil stand high above the chaotic scablands. Constrictions at several places caused the floodwaters to pool into large temporary lakes, such as Lake Lewis , in which sediments were deposited. Water depths have been estimated at 1,000 feet (300 m) at Wallula Gap and 400 feet (120 m) over modern Portland, Oregon. Sediments were also deposited when
1036-426: A dam and reservoir is a flexible source, since the amount of electricity produced can be increased or decreased in seconds or minutes in response to varying electricity demand. Once a hydroelectric complex is constructed, it produces no direct waste, and almost always emits considerably less greenhouse gas than fossil fuel -powered energy plants. However, when constructed in lowland rainforest areas, where part of
1184-421: A flood and fail. Changes in the amount of river flow will correlate with the amount of energy produced by a dam. Lower river flows will reduce the amount of live storage in a reservoir therefore reducing the amount of water that can be used for hydroelectricity. The result of diminished river flow can be power shortages in areas that depend heavily on hydroelectric power. The risk of flow shortage may increase as
1332-809: A large natural height difference between two waterways, such as a waterfall or mountain lake. A tunnel is constructed to take water from the high reservoir to the generating hall built in a cavern near the lowest point of the water tunnel and a horizontal tailrace taking water away to the lower outlet waterway. A simple formula for approximating electric power production at a hydroelectric station is: P = − η ( m ˙ g Δ h ) = − η ( ( ρ V ˙ ) g Δ h ) {\displaystyle P=-\eta \ ({\dot {m}}g\ \Delta h)=-\eta \ ((\rho {\dot {V}})\ g\ \Delta h)} where Efficiency
1480-451: A larger amount of methane than those in temperate areas. Like other non-fossil fuel sources, hydropower also has no emissions of sulfur dioxide, nitrogen oxides, or other particulates. Reservoirs created by hydroelectric schemes often provide facilities for water sports , and become tourist attractions themselves. In some countries, aquaculture in reservoirs is common. Multi-use dams installed for irrigation support agriculture with
1628-734: A physician who had been in the fur trade since 1804, was appointed superintendent of the Columbia District. The HBC reoriented its Columbia District operations toward the Pacific Ocean via the Columbia, which became the region's main trunk route. In the early 1840s Americans began to colonize the Oregon country in large numbers via the Oregon Trail , despite the HBC's efforts to discourage American settlement in
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#17328554570641776-520: A population as great as 10,000. The site drew traders from as far away as the Great Plains. The Cascades Rapids of the Columbia River Gorge, and Kettle Falls and Priest Rapids in eastern Washington, were also major fishing and trading sites. In prehistoric times the Columbia's salmon and steelhead runs numbered an estimated annual average of 10 to 16 million fish. In comparison,
1924-586: A positive risk adjusted return, unless appropriate risk management measures are put in place. While many hydroelectric projects supply public electricity networks, some are created to serve specific industrial enterprises. Dedicated hydroelectric projects are often built to provide the substantial amounts of electricity needed for aluminium electrolytic plants, for example. The Grand Coulee Dam switched to support Alcoa aluminium in Bellingham, Washington , United States for American World War II airplanes before it
2072-681: 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
2220-545: A relatively constant water supply. Large hydro dams can control floods, which would otherwise affect people living downstream of the project. Managing dams which are also used for other purposes, such as irrigation , is complicated. In 2021 the IEA called for "robust sustainability standards for all hydropower development with streamlined rules and regulations". Large reservoirs associated with traditional hydroelectric power stations result in submersion of extensive areas upstream of
2368-470: A result of climate change . One study from the Colorado River in the United States suggest that modest climate changes, such as an increase in temperature in 2 degree Celsius resulting in a 10% decline in precipitation, might reduce river run-off by up to 40%. Brazil in particular is vulnerable due to its heavy reliance on hydroelectricity, as increasing temperatures, lower water flow and alterations in
2516-471: A shifting sandbar that makes the river's mouth one of the most hazardous stretches of water to navigate in the world. Because of the danger and the many shipwrecks near the mouth, it acquired a reputation as the "Graveyard of Ships". The Columbia drains an area of about 258,000 sq mi (670,000 km ). Its drainage basin covers nearly all of Idaho , large portions of British Columbia, Oregon, and Washington, and ultimately all of Montana west of
2664-448: A small TV/radio). Even smaller turbines of 200–300 W may power a few homes in a developing country with a drop of only 1 m (3 ft). A Pico-hydro setup is typically run-of-the-river , meaning that dams are not used, but rather pipes divert some of the flow, drop this down a gradient, and through the turbine before returning it to the stream. An underground power station is generally used at large facilities and makes use of
2812-455: A source of low-cost renewable energy. Alternatively, small hydro projects may be built in isolated areas that would be uneconomic to serve from a grid, or in areas where there is no national electrical distribution network. Since small hydro projects usually have minimal reservoirs and civil construction work, they are seen as having a relatively low environmental impact compared to large hydro. This decreased environmental impact depends strongly on
2960-414: A start-up time of the order of a few minutes. Although battery power is quicker its capacity is tiny compared to hydro. It takes less than 10 minutes to bring most hydro units from cold start-up to full load; this is quicker than nuclear and almost all fossil fuel power. Power generation can also be decreased quickly when there is a surplus power generation. Hence the limited capacity of hydropower units
3108-436: A temporary camp was set up on the bottom of the gorge, and exploratory drilling work commenced in 1951. The work at the lower site at river mile 39.5 left two drifts measuring about 5 feet (1.5 m) by 7 feet (2.1 m) and about 50 feet (15 m) deep in the cliffs on either side of the river, together with 32 drill holes in the river bed. At the upper site, about 7 miles (11 km) upstream at river mile 32.8, there were
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#17328554570643256-581: A total of 1,500 terawatt-hours (TWh) of electrical energy in one full cycle" which was "about 170 times more energy than the global fleet of pumped storage hydropower plants". Battery storage capacity is not expected to overtake pumped storage during the 2020s. When used as peak power to meet demand, hydroelectricity has a higher value than baseload power and a much higher value compared to intermittent energy sources such as wind and solar. Hydroelectric stations have long economic lives, with some plants still in service after 50–100 years. Operating labor cost
3404-408: A total of 35 drill holes and two drifts 100 feet (30 m) and 75 feet (23 m) deep. The work sites were accessed by an aerial tram from the rim. Although the lower site was preferred due to an additional 30 feet (9.1 m) of hydraulic head and potentially 45% larger reservoir than was possible at the upper site, it required more work to remediate weak rock joints. The project was not pursued by
3552-596: A year's worth of rain fell within 24 hours (see 1975 Banqiao Dam failure ). The resulting flood resulted in the deaths of 26,000 people, and another 145,000 from epidemics. Millions were left homeless. The creation of a dam in a geologically inappropriate location may cause disasters such as 1963 disaster at Vajont Dam in Italy, where almost 2,000 people died. Columbia River The Columbia River ( Upper Chinook : Wimahl or Wimal ; Sahaptin : Nch’i-Wàna or Nchi wana ; Sinixt dialect swah'netk'qhu )
3700-533: Is Hanford Reach , the only U.S. stretch of the river that is completely free-flowing, unimpeded by dams, and not a tidal estuary . The Snake River and Yakima River join the Columbia in the Tri-Cities population center. The Columbia makes a sharp bend to the west at the Washington–Oregon border. The river defines that border for the final 309 mi (497 km) of its journey. The Deschutes River joins
3848-435: Is electricity generated from hydropower (water power). Hydropower supplies 15% of the world's electricity , almost 4,210 TWh in 2023, which is more than all other renewable sources combined and also more than nuclear power . Hydropower can provide large amounts of low-carbon electricity on demand, making it a key element for creating secure and clean electricity supply systems. A hydroelectric power station that has
3996-448: Is hydroelectric power on a scale serving a small community or industrial plant. The definition of a small hydro project varies but a generating capacity of up to 10 megawatts (MW) is generally accepted as the upper limit. This may be stretched to 25 MW and 30 MW in Canada and the United States. Small hydro stations may be connected to conventional electrical distribution networks as
4144-627: Is also usually low, as plants are automated and have few personnel on site during normal operation. Where a dam serves multiple purposes, a hydroelectric station may be added with relatively low construction cost, providing a useful revenue stream to offset the costs of dam operation. It has been calculated that the sale of electricity from the Three Gorges Dam will cover the construction costs after 5 to 8 years of full generation. However, some data shows that in most countries large hydropower dams will be too costly and take too long to build to deliver
4292-466: Is highest in the winter when solar energy is at a minimum. Pico hydro is hydroelectric power generation of under 5 kW . It is useful in small, remote communities that require only a small amount of electricity. For example, the 1.1 kW Intermediate Technology Development Group Pico Hydro Project in Kenya supplies 57 homes with very small electric loads (e.g., a couple of lights and a phone charger, or
4440-445: Is initially produced during construction of the project, and some methane is given off annually by reservoirs, hydro has one of the lowest lifecycle greenhouse gas emissions for electricity generation. The low greenhouse gas impact of hydroelectricity is found especially in temperate climates . Greater greenhouse gas emission impacts are found in the tropical regions because the reservoirs of power stations in tropical regions produce
4588-661: Is not federally recognized , who live near the lower Columbia River, call it Wimahl or Wimal in the Upper Chinook (Kiksht) language , and it is Nch’i-Wàna or Nchi wana to the Sahaptin (Ichishkíin Sɨ́nwit) -speaking peoples of its middle course in present-day Washington. The river is known as swah'netk'qhu by the Sinixt people , who live in the area of the Arrow Lakes in
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4736-462: Is not an energy source, and appears as a negative number in listings. Run-of-the-river hydroelectric stations are those with small or no reservoir capacity, so that only the water coming from upstream is available for generation at that moment, and any oversupply must pass unused. A constant supply of water from a lake or existing reservoir upstream is a significant advantage in choosing sites for run-of-the-river. A tidal power station makes use of
4884-452: Is not generally used to produce base power except for vacating the flood pool or meeting downstream needs. Instead, it can serve as backup for non-hydro generators. The major advantage of conventional hydroelectric dams with reservoirs is their ability to store water at low cost for dispatch later as high value clean electricity. In 2021, the IEA estimated that the "reservoirs of all existing conventional hydropower plants combined can store
5032-410: Is often higher (that is, closer to 1) with larger and more modern turbines. Annual electric energy production depends on the available water supply. In some installations, the water flow rate can vary by a factor of 10:1 over the course of a year. Hydropower is a flexible source of electricity since stations can be ramped up and down very quickly to adapt to changing energy demands. Hydro turbines have
5180-518: 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
5328-599: 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
5476-871: The Big Bend Country , passing through Revelstoke Lake and the Arrow Lakes . Revelstoke, the Big Bend, and the Columbia Valley combined are referred to in BC parlance as the Columbia Country . Below the Arrow Lakes, the Columbia passes the cities of Castlegar , located at the Columbia's confluence with the Kootenay River , and Trail , two major population centers of the West Kootenay region. The Pend Oreille River joins
5624-657: The Bonneville Dam in 1937 and being recognized by the Flood Control Act of 1936 as the premier federal flood control agency. Hydroelectric power stations continued to become larger throughout the 20th century. Hydropower was referred to as "white coal". Hoover Dam 's initial 1,345 MW power station was the world's largest hydroelectric power station in 1936; it was eclipsed by the 6,809 MW Grand Coulee Dam in 1942. The Itaipu Dam opened in 1984 in South America as
5772-646: The Canadian Rockies and the Columbia Mountains in BC. For its first 200 mi (320 km), the Columbia flows northwest along the trench through Windermere Lake and the town of Invermere , a region known in BC as the Columbia Valley , then northwest to Golden and into Kinbasket Lake . Rounding the northern end of the Selkirk Mountains , the river turns sharply south through a region known as
5920-547: The Columbia River Plateau and forced the lower Columbia into its present course. The modern Cascade Range began to uplift 5 to 4 million years ago. Cutting through the uplifting mountains, the Columbia River significantly deepened the Columbia River Gorge. The river and its drainage basin experienced some of the world's greatest known catastrophic floods toward the end of the last ice age . The periodic rupturing of ice dams at Glacial Lake Missoula resulted in
6068-576: The Continental Divide , and small portions of Wyoming , Utah , and Nevada ; the total area is similar to the size of France. Roughly 745 mi (1,199 km) of the river's length and 85 percent of its drainage basin are in the US. The Columbia is the twelfth-longest river and has the sixth-largest drainage basin in the United States. In Canada, where the Columbia flows for 498 mi (801 km) and drains 39,700 sq mi (103,000 km ),
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6216-702: The Eocene through the Miocene eras, tremendous volcanic eruptions frequently modified much of the landscape traversed by the Columbia. The lower reaches of the ancestral river passed through a valley near where Mount Hood later arose. Carrying sediments from erosion and erupting volcanoes, it built a 2-mile (3.2 km) thick delta that underlies the foothills on the east side of the Coast Range near Vernonia in northwestern Oregon. Between 17 million and 6 million years ago, huge outpourings of flood basalt lava covered
6364-581: The Grand Coulee Dam in the mid-20th century impounded the river, forming Lake Roosevelt , from which water was pumped into the dry coulee , forming the reservoir of Banks Lake . The river flows past The Gorge Amphitheatre , a prominent concert venue in the Northwest, then through Priest Rapids Dam , and then through the Hanford Nuclear Reservation . Entirely within the reservation
6512-533: The Industrial Revolution would drive development as well. In 1878, the world's first hydroelectric power scheme was developed at Cragside in Northumberland , England, by William Armstrong . It was used to power a single arc lamp in his art gallery. The old Schoelkopf Power Station No. 1 , US, near Niagara Falls , began to produce electricity in 1881. The first Edison hydroelectric power station,
6660-778: The International Exhibition of Hydropower and Tourism , with over one million visitors 1925. By 1920, when 40% of the power produced in the United States was hydroelectric, the Federal Power Act was enacted into law. The Act created the Federal Power Commission to regulate hydroelectric power stations on federal land and water. As the power stations became larger, their associated dams developed additional purposes, including flood control , irrigation and navigation . Federal funding became necessary for large-scale development, and federally owned corporations, such as
6808-607: The Marmes Rockshelter , near the confluence of the Palouse and Snake rivers in eastern Washington. In 1996 the skeletal remains of a 9,000-year-old prehistoric man (dubbed Kennewick Man ) were found near Kennewick, Washington . The discovery rekindled debate in the scientific community over the origins of human habitation in North America and sparked a protracted controversy over whether the scientific or Native American community
6956-600: The Missouri River . The first documented European discovery of the Columbia River was that of Bruno de Heceta , who in 1775 sighted the river's mouth. On the advice of his officers, he did not explore it, as he was short-staffed and the current was strong. He considered it a bay, and called it Ensenada de Asunción ( Assumption Cove ). Later Spanish maps, based on his sighting, showed a river, labeled Río de San Roque ( The Saint Roch River ), or an entrance, called Entrada de Hezeta , named for Bruno de Hezeta , who sailed
7104-548: The Molala , Klickitat , Wenatchi , Okanagan, and Sinkiuse-Columbia peoples, who owned small numbers of horses and adopted few plains culture features. Some groups remained essentially unaffected, such as the Sanpoil and Nespelem people, whose culture remained centered on fishing. Natives of the region encountered foreigners at several times and places during the 18th and 19th centuries. European and American vessels explored
7252-517: The Oregon Country along the Clearwater and Snake rivers, and encountered numerous small settlements of natives. Their records recount tales of hospitable traders who were not above stealing small items from the visitors. They also noted brass teakettles, a British musket, and other artifacts that had been obtained in trade with coastal tribes. From the earliest contact with westerners, the natives of
7400-763: The Shoshone Bannock tribes are present. The Sinixt or Lakes people lived on the lower stretch of the Canadian portion, while above that the Shuswap people (Secwepemc in their own language) reckon the whole of the upper Columbia east to the Rockies as part of their territory. The Canadian portion of the Columbia Basin outlines the traditional homelands of the Canadian Kootenay– Ktunaxa . The Chinook tribe, which
7548-605: The Tennessee Valley Authority (1933) and the Bonneville Power Administration (1937) were created. Additionally, the Bureau of Reclamation which had begun a series of western US irrigation projects in the early 20th century, was now constructing large hydroelectric projects such as the 1928 Hoover Dam . The United States Army Corps of Engineers was also involved in hydroelectric development, completing
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#17328554570647696-569: The Vulcan Street Plant , began operating September 30, 1882, in Appleton, Wisconsin , with an output of about 12.5 kilowatts. By 1886 there were 45 hydroelectric power stations in the United States and Canada; and by 1889 there were 200 in the United States alone. At the beginning of the 20th century, many small hydroelectric power stations were being constructed by commercial companies in mountains near metropolitan areas. Grenoble , France held
7844-473: The Yakima War , decimated the native population and removed much land from native control. As years progressed, the right of natives to fish along the Columbia became the central issue of contention with the states, commercial fishers, and private property owners. The US Supreme Court upheld fishing rights in landmark cases in 1905 and 1918, as well as the 1974 case United States v. Washington , commonly called
7992-455: The eruption of Mount St. Helens deposited large amounts of sediment in the lower Columbia, temporarily reducing the depth of the shipping channel by 26 feet (7.9 m). Humans have inhabited the Columbia's watershed for more than 15,000 years, with a transition to a sedentary lifestyle based mainly on salmon starting about 3,500 years ago. In 1962, archaeologists found evidence of human activity dating back 11,230 years at
8140-506: The potential energy of dammed water driving a water turbine and generator . The power extracted from the water depends on the volume and on the difference in height between the source and the water's outflow. This height difference is called the head . A large pipe (the " penstock ") delivers water from the reservoir to the turbine. This method produces electricity to supply high peak demands by moving water between reservoirs at different elevations. At times of low electrical demand,
8288-400: The water frame , and continuous production played a significant part in the development of the factory system, with modern employment practices. In the 1840s, hydraulic power networks were developed to generate and transmit hydro power to end users. By the late 19th century, the electrical generator was developed and could now be coupled with hydraulics. The growing demand arising from
8436-534: The 1840s a mass migration of American settlers undermined British control. The Hudson's Bay Company tried to maintain dominance by shifting from the fur trade, which was in decline, to exporting other goods such as salmon and lumber. Colonization schemes were attempted, but failed to match the scale of American settlement. Americans generally settled south of the Columbia, mainly in the Willamette Valley. The Hudson's Bay Company tried to establish settlements north of
8584-452: The 1930s, there were natives who lived along the river and fished year round, moving along with the fish's migration patterns throughout the seasons. The Yakama were slower to do so, organizing a formal government in 1944. In the 21st century, the Yakama, Nez Perce, Umatilla, and Warm Springs tribes all have treaty fishing rights along the Columbia and its tributaries. In 1957 Celilo Falls
8732-473: The 20th century, each of these major fishing sites was flooded by a dam, beginning with Cascades Rapids in 1938. The development was accompanied by extensive negotiations between natives and US government agencies. The Confederated Tribes of Warm Springs, a coalition of various tribes, adopted a constitution and incorporated after the 1938 completion of the Bonneville Dam flooded Cascades Rapids; Still, in
8880-460: The Americas and is the fourth-largest by volume in the U.S. The average flow where the river crosses the international border between Canada and the United States is 2,790 m /s (99,000 cu ft/s) from a drainage basin of 102,800 km (39,700 sq mi). This amounts to about 15 percent of the entire Columbia watershed. The Columbia's highest recorded flow, measured at The Dalles,
9028-594: The Boldt Decision. Fish were central to the culture of the region's natives, both as sustenance and as part of their religious beliefs. Natives drew fish from the Columbia at several major sites, which also served as trading posts. Celilo Falls , located east of the modern city of The Dalles, was a vital hub for trade and the interaction of different cultural groups, being used for fishing and trading for 11,000 years. Prior to contact with westerners, villages along this 9-mile (14 km) stretch may have at times had
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#17328554570649176-616: The Bureau of Reclamation in the 1950s. In 1960 the Arizona Power Authority became interested in the site, whose reservoir would have been entirely in Arizona, giving the state control over the waters and power generation. In 1963 the effort was endorsed by Bureau of Reclamation director Floyd Dominy . Investigations for the project's feasibility report extended into 1964. In 1965 a Bureau of Reclamation report concluded that solution cavities in
9324-541: The Colorado River. The Bureau had even grander visions, too: eventually, this generated revenue would be necessary to fund water import projects from the Columbia River system to the Colorado River, which continues to face shortages due to over-appropriation of its flow. Thus, "hydropower at Bridge and Marble Canyon Dams was viewed as an instrument and not as a major goal in itself". The feasibility of Marble Canyon Dam
9472-489: The Columbia Bar, becoming the first known explorer of European descent to enter the river . Gray's fur trading mission had been financed by Boston merchants, who outfitted him with a private vessel named Columbia Rediviva ; he named the river after the ship on May 18. Gray spent nine days trading near the mouth of the Columbia, then left without having gone beyond 13 miles (21 km) upstream. The farthest point reached
9620-486: The Columbia River Gorge, about 100 miles (160 km) upstream, sighting and naming Mount Hood. Broughton formally claimed the river, its drainage basin , and the nearby coast for Britain. In contrast, Gray had not made any formal claims on behalf of the United States. Because the Columbia was at the same latitude as the headwaters of the Missouri River, there was some speculation that Gray and Vancouver had discovered
9768-538: The Columbia River Gorge, sending massive amounts of debris south from Table Mountain and Greenleaf Peak into the gorge near the present site of Bonneville Dam. The most recent and significant is known as the Bonneville Slide , which formed a massive earthen dam, filling 3.5 miles (5.6 km) of the river's length. Various studies have placed the date of the Bonneville Slide anywhere between 1060 and 1760 AD;
9916-417: The Columbia River Gorge. The Celilo Canal , bypassing Celilo Falls, opened to river traffic in 1915. In the mid-20th century, the construction of dams along the length of the river submerged the rapids beneath a series of reservoirs. An extensive system of locks allowed ships and barges to pass easily between reservoirs. A navigation channel reaching Lewiston, Idaho , along the Columbia and Snake rivers,
10064-478: The Columbia River. The mountainous terrain where the unit would be placed in is Juniper Point, referred to by the Yakama as Pushpum. Pushpum has rock formations, as well as food and medicine capabilities that are essential to the Yakama. Members of the Yakama tribe wish for consent on the Goldendale project, as opposed to consultation. Some historians believe that Japanese or Chinese vessels blown off course reached
10212-424: The Columbia about 2 miles (3 km) north of the United States–Canada border . The Columbia enters eastern Washington flowing south and turning to the west at the Spokane River confluence. It marks the southern and eastern borders of the Colville Indian Reservation and the western border of the Spokane Indian Reservation . The river turns south after the Okanogan River confluence, then southeasterly near
10360-407: 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
10508-412: The Columbia near The Dalles . Between The Dalles and Portland , the river cuts through the Cascade Range , forming the dramatic Columbia River Gorge . Via the gorge, the Columbia crosses the Cascades at a lower elevation than any other river. The gorge is known for its strong and steady winds, scenic beauty, and its role as an important transportation link. The river continues west, bending sharply to
10656-406: The Columbia to improve navigation. Changes to the river over the years have included the construction of jetties at the river's mouth, dredging , and the construction of canals and navigation locks . Today, ocean freighters can travel upriver as far as Portland and Vancouver, and barges can reach as far inland as Lewiston, Idaho . The shifting Columbia Bar makes passage between the river and
10804-481: 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
10952-457: The Columbia, they failed to send word home to Spain. In the 18th century, there was strong interest in discovering a Northwest Passage that would permit navigation between the Atlantic (or inland North America) and the Pacific Ocean. Many ships in the area, especially those under Spanish and British command, searched the northwest coast for a large river that might connect to Hudson Bay or
11100-585: The Hoover Dam, which would provide a much greater storage capacity for irrigation and flood control. However, once Hoover was completed the Bureau once again set its sights on the Grand Canyon, which has the greatest hydroelectric potential of any canyon in the American Southwest. In the late 1940s, crews led by Bureau engineer Bert Lucas began to survey Marble Canyon and identified at least two suitable dam sites, one 32.8 miles (52.8 km) below Lee's Ferry and
11248-463: The IEA released a main-case forecast of 141 GW generated by hydropower over 2022–2027, which is slightly lower than deployment achieved from 2017–2022. Because environmental permitting and construction times are long, they estimate hydropower potential will remain limited, with only an additional 40 GW deemed possible in the accelerated case. In 2021 the IEA said that major modernisation refurbishments are required. Most hydroelectric power comes from
11396-758: The Lower Umpqua Tribe, Siuslaw Tribe, and Coos Tribe in 1984, the Klamath Tribe in 1986, and the Coquille Tribe in 1989. While all the aforementioned tribes received federally recognized status, the Chinook Indian Nation had their federal recognition revoked in 2002 by the Bush Administration, and are fighting to have it restored. In 2023, members of the Yakama Nation expressed their dismay for
11544-469: The Missoula Floods, with discharges exceeding the combined flow of all the other rivers in the world, dozens of times over thousands of years. The exact number of floods is unknown, but geologists have documented at least 40; evidence suggests that they occurred between about 19,000 and 13,000 years ago. The floodwaters rushed across eastern Washington, creating the channeled scablands , which are
11692-525: The Northwest Coast long before Europeans—possibly as early as 219 BCE . Historian Derek Hayes claims that "It is a near certainty that Japanese or Chinese people arrived on the northwest coast long before any European." It is unknown whether they landed near the Columbia. Evidence exists that Spanish castaways reached the shore in 1679 and traded with the Clatsop ; if these were the first Europeans to see
11840-421: The Pacific Ocean difficult and dangerous, and numerous rapids along the river hinder navigation. Pacific Graveyard, a 1964 book by James A. Gibbs , describes the many shipwrecks near the mouth of the Columbia. Jetties, first constructed in 1886, extend the river's channel into the ocean. Strong currents and the shifting sandbar remain a threat to ships entering the river and necessitate continuous maintenance of
11988-521: The Snake River, reaching the Columbia near the present-day Tri-Cities, Washington. They explored a few miles upriver, as far as Bateman Island , before heading down the Columbia, concluding their journey at the river's mouth and establishing Fort Clatsop , a short-lived establishment that was occupied for less than three months. Canadian explorer David Thompson , of the North West Company , spent
12136-704: The Union in 1889. By the turn of the 20th century, the difficulty of navigating the Columbia was seen as an impediment to the economic development of the Inland Empire region east of the Cascades. The dredging and dam building that followed would permanently alter the river, disrupting its natural flow but also providing electricity, irrigation , navigability and other benefits to the region. American captain Robert Gray and British captain George Vancouver, who explored
12284-409: The United States. A number of accessory lakes or pools were projected in the adjacent Deer Creek drainage, or possibly at a 450-foot (140 m) dam on Kanab Creek. The power station at Deer Creek would have been at the head of the reservoir backed up by the never-built Bridge Canyon Dam . By the 1960s the tunnel project had been dropped in favor of a 600 MW power station at the dam's base, reducing
12432-504: The Yakama Tribe were arrested in a federal sting operation which claimed that fishermen were poaching up to 40,000 fish in the Columbia River. Fishermen placed on trial received sentences ranging from six months to five years. The federal government pinned Yakama Tribe member David Sohappy ringleader of the operation. After the trial ended, it was determined that the fish were not poached, but driven away because of harmful chemicals present in
12580-464: The ability to transport particles heavier than itself downstream. This has a negative effect on dams and subsequently their power stations, particularly those on rivers or within catchment areas with high siltation. Siltation can fill a reservoir and reduce its capacity to control floods along with causing additional horizontal pressure on the upstream portion of the dam. Eventually, some reservoirs can become full of sediment and useless or over-top during
12728-650: The affection of a goddess, represented by Mount St. Helens . Native American stories about the bridge differ in their details but agree in general that the bridge permitted increased interaction between tribes on the north and south sides of the river. Horses, originally acquired from Spanish New Mexico , spread widely via native trade networks, reaching the Shoshone of the Snake River Plain by 1700. The Nez Perce, Cayuse, and Flathead people acquired their first horses around 1730. Along with horses came aspects of
12876-595: The balance between stream flow and power production. Micro hydro means hydroelectric power installations that typically produce up to 100 kW of power. These installations can provide power to an isolated home or small community, or are sometimes connected to electric power networks. There are many of these installations around the world, particularly in developing nations as they can provide an economical source of energy without purchase of fuel. Micro hydro systems complement photovoltaic solar energy systems because in many areas water flow, and thus available hydro power,
13024-645: The base of Bonneville Dam , its head of tide . When the rifting of Pangaea , due to the process of plate tectonics , pushed North America away from Europe and Africa and into the Panthalassic Ocean (ancestor to the modern Pacific Ocean), the Pacific Northwest was not part of the continent. As the North American continent moved westward, the Farallon Plate subducted under its western margin. As
13172-518: The center of an extensive trading network across the Pacific Plateau. Celilo was the oldest continuously inhabited community on the North American continent. Salmon canneries established by white settlers beginning in 1866 had a strong negative impact on the salmon population, and in 1908 US president Theodore Roosevelt observed that the salmon runs were but a fraction of what they had been 25 years prior. As river development continued in
13320-466: The coastal area around the mouth of the river in the late 18th century, trading with local natives. The contact would prove devastating to the indigenous Chinookan speaking peoples; a large portion of their population was wiped out by a smallpox epidemic. Canadian explorer Alexander Mackenzie crossed what is now interior British Columbia in 1793. From 1805 to 1806, the Lewis and Clark Expedition entered
13468-633: The confluence with the Wenatchee River in central Washington. This C-shaped segment of the river is also known as the "Big Bend". During the Missoula Floods 10–15,000 years ago, much of the floodwater took a more direct route south, forming the ancient river bed known as the Grand Coulee . After the floods, the river found its present course, and the Grand Coulee was left dry. The construction of
13616-449: The construction of a Goldendale-based pumped hydroelectric energy storage project. Jeremy Takala of the Yakama Nation embodies Yakama belief on the importance of Columbia River crops to food and medicine, stating "the [Goldendale] project being proposed here, it will definitely impact our life". The Goldendale-pumped hydro storage unit could allow for reused water use in reservoirs, which would be placed on mountainous terrain overlooking
13764-404: The daily rise and fall of ocean water due to tides; such sources are highly predictable, and if conditions permit construction of reservoirs, can also be dispatchable to generate power during high demand periods. Less common types of hydro schemes use water's kinetic energy or undammed sources such as undershot water wheels . Tidal power is viable in a relatively small number of locations around
13912-505: The dams, sometimes destroying biologically rich and productive lowland and riverine valley forests, marshland and grasslands. Damming interrupts the flow of rivers and can harm local ecosystems, and building large dams and reservoirs often involves displacing people and wildlife. The loss of land is often exacerbated by habitat fragmentation of surrounding areas caused by the reservoir. Hydroelectric projects can be disruptive to surrounding aquatic ecosystems both upstream and downstream of
14060-690: The effect of forest decay. Another disadvantage of hydroelectric dams is the need to relocate the people living where the reservoirs are planned. In 2000, the World Commission on Dams estimated that dams had physically displaced 40–80 million people worldwide. Because large conventional dammed-hydro facilities hold back large volumes of water, a failure due to poor construction, natural disasters or sabotage can be catastrophic to downriver settlements and infrastructure. During Typhoon Nina in 1975 Banqiao Dam in Southern China failed when more than
14208-468: The emerging plains culture , such as equestrian and horse training skills, greatly increased mobility, hunting efficiency, trade over long distances, intensified warfare, the linking of wealth and prestige to horses and war, and the rise of large and powerful tribal confederacies. The Nez Perce and Cayuse kept large herds and made annual long-distance trips to the Great Plains for bison hunting, adopted
14356-399: The excess generation capacity is used to pump water into the higher reservoir, thus providing demand side response . When the demand becomes greater, water is released back into the lower reservoir through a turbine. In 2021 pumped-storage schemes provided almost 85% of the world's 190 GW of grid energy storage and improve the daily capacity factor of the generation system. Pumped storage
14504-452: The floodwaters slowed in the broad flats of the Quincy, Othello, and Pasco Basins. The floods' periodic inundation of the lower Columbia River Plateau deposited rich sediments; 21st-century farmers in the Willamette Valley "plow fields of fertile Montana soil and clays from Washington's Palouse". Over the last several thousand years a series of large landslides have occurred on the north side of
14652-534: The forest is inundated, substantial amounts of greenhouse gases may be emitted. Construction of a hydroelectric complex can have significant environmental impact, principally in loss of arable land and population displacement. They also disrupt the natural ecology of the river involved, affecting habitats and ecosystems, and siltation and erosion patterns. While dams can ameliorate the risks of flooding, dam failure can be catastrophic. In 2021, global installed hydropower electrical capacity reached almost 1,400 GW,
14800-506: The highest among all renewable energy technologies. Hydroelectricity plays a leading role in countries like Brazil, Norway and China. but there are geographical limits and environmental issues. Tidal power can be used in coastal regions. China added 24 GW in 2022, accounting for nearly three-quarters of global hydropower capacity additions. Europe added 2 GW, the largest amount for the region since 1990. Meanwhile, globally, hydropower generation increased by 70 TWh (up 2%) in 2022 and remains
14948-427: The idea that the landslide debris present today was formed by more than one slide is relatively recent and may explain the large range of estimates. It has been suggested that if the later dates are accurate there may be a link with the 1700 Cascadia earthquake . The pile of debris resulting from the Bonneville Slide blocked the river until rising water finally washed away the sediment. It is not known how long it took
15096-518: The jetties. In 1891, the Columbia was dredged to enhance shipping. The channel between the ocean and Portland and Vancouver was deepened from 17 feet (5.2 m) to 25 feet (7.6 m). The Columbian called for the channel to be deepened to 40 feet (12 m) as early as 1905, but that depth was not attained until 1976. Cascade Locks and Canal were first constructed in 1896 around the Cascades Rapids, enabling boats to travel safely through
15244-519: The largest renewable energy source, surpassing all other technologies combined. Hydropower has been used since ancient times to grind flour and perform other tasks. In the late 18th century hydraulic power provided the energy source needed for the start of the Industrial Revolution . In the mid-1700s, French engineer Bernard Forest de Bélidor published Architecture Hydraulique , which described vertical- and horizontal-axis hydraulic machines, and in 1771 Richard Arkwright 's combination of water power ,
15392-447: The largest run since 1938 was in 1986, with 3.2 million fish entering the Columbia. The annual catch by natives has been estimated at 42 million pounds (19,000 metric tons). The most important and productive native fishing site was located at Celilo Falls, which was perhaps the most productive inland fishing site in North America. The falls were located at the border between Chinookan- and Sahaptian-speaking peoples and served as
15540-731: The largest, producing 14 GW , but was surpassed in 2008 by the Three Gorges Dam in China at 22.5 GW . Hydroelectricity would eventually supply some countries, including Norway , Democratic Republic of the Congo , Paraguay and Brazil , with over 85% of their electricity. In 2021 the International Energy Agency (IEA) said that more efforts are needed to help limit climate change . Some countries have highly developed their hydropower potential and have very little room for growth: Switzerland produces 88% of its potential and Mexico 80%. In 2022,
15688-442: 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
15836-462: The location in Marble Canyon was regarded as one of the most remote and difficult-to-access dam sites in the United States, about 2,500 feet (760 m) below the rim of the canyon. The proposed dam was of moderate size, about 310 feet (94 m) high, using a thin-arch concrete design and retaining about 363,000 acre-feet. To keep the small reservoir free of silt, silt retention dams were needed on
15984-577: The long-sought Northwest Passage. A 1798 British map showed a dotted line connecting the Columbia with the Missouri. When the American explorers Meriwether Lewis and William Clark charted the vast, unmapped lands of the American West in their overland expedition (1803–1805), they found no passage between the rivers. After crossing the Rocky Mountains , Lewis and Clark built dugout canoes and paddled down
16132-464: The mid- and lower Columbia were not tribal, but instead congregated in social units no larger than a village, and more often at a family level; these units would shift with the season as people moved about, following the salmon catch up and down the river's tributaries. Sparked by the 1847 Whitman Massacre , a number of violent battles were fought between American settlers and the region's natives. The subsequent wars over Northwest territory, especially
16280-580: The north-northwest near Portland and Vancouver, Washington , at the Willamette River confluence. Here the river slows considerably, dropping sediment that might otherwise form a river delta at the Columbia's mouth. Near Longview, Washington and the Cowlitz River confluence, the river turns west again. The Columbia empties into the Pacific Ocean just west of Astoria, Oregon , over the Columbia Bar ,
16428-467: The plains culture to a significant degree, and became the main conduit through which horses and the plains culture diffused into the Columbia River region. Other peoples acquired horses and aspects of the plains culture unevenly. The Yakama, Umatilla, Palus, Spokane, and Coeur d'Alene maintained sizable herds of horses and adopted some of the plains cultural characteristics, but fishing and fish-related economies remained important. Less affected groups included
16576-633: The plant site. Generation of hydroelectric power changes the downstream river environment. Water exiting a turbine usually contains very little suspended sediment, which can lead to scouring of river beds and loss of riverbanks. The turbines also will kill large portions of the fauna passing through, for instance 70% of the eel passing a turbine will perish immediately. Since turbine gates are often opened intermittently, rapid or even daily fluctuations in river flow are observed. Drought and seasonal changes in rainfall can severely limit hydropower. Water may also be lost by evaporation. When water flows it has
16724-415: The plate subducted, it carried along island arcs which were accreted to the North American continent, resulting in the creation of the Pacific Northwest between 150 and 90 million years ago. The general outline of the Columbia Basin was not complete until between 60 and 40 million years ago, but it lay under a large inland sea later subject to uplift. Between 50 and 20 million years ago, from
16872-550: The possibility of a dam in Marble Canyon. In 1975 the monument was added to Grand Canyon National Park by the Grand Canyon Enlargement Act. The lower dam would have flooded a number of natural features, including Redwall Cavern and Vasey's Paradise. The upper dam was located just above the cavern, and was sometimes referred to as Redwall Dam. Hydroelectricity Hydroelectricity , or hydroelectric power ,
17020-688: The power plant. These harmful chemicals mainly consisted of aluminum. This event is commonly known today as the Salmon Scam . Shortly after the Salmon Scam, many Columbia River-based indigenous tribes received federally recognized status. The Siletz Tribe was the first to restore its federal recognition in 1977, followed by the Cow Creek Band of the Umpqua Tribe in 1982, the Grand Ronde Tribe in 1983,
17168-591: The project's costs considerably. The two dams would be operated as "cash register" power plants, meaning that sale of hydroelectricity would pay for their construction cost as well as provide funds for future reclamation projects. The power thus produced would be vital for pumping along the Central Arizona Project (CAP), which would lift water from the Colorado River near Lake Havasu to central and southern Arizona. The pumped water would reach as far as Tucson , which sits about 2,000 feet (610 m) higher than
17316-450: The rainfall regime, could reduce total energy production by 7% annually by the end of the century. Lower positive impacts are found in the tropical regions. In lowland rainforest areas, where inundation of a part of the forest is necessary, it has been noted that the reservoirs of power plants produce substantial amounts of methane . This is due to plant material in flooded areas decaying in an anaerobic environment and forming methane,
17464-735: The rapid settlement and economic development of the region. Steamboats operated in several distinct stretches of the river: on its lower reaches, from the Pacific Ocean to Cascades Rapids; from the Cascades to the Dalles-Celilo Falls; from Celilo to Priests Rapids; on the Wenatchee Reach of eastern Washington; on British Columbia's Arrow Lakes ; and on tributaries like the Willamette , the Snake and Kootenay Lake . The boats, initially powered by burning wood, carried passengers and freight throughout
17612-460: The region for many years. Early railroads served to connect steamboat lines interrupted by waterfalls on the river's lower reaches. In the 1880s, railroads maintained by companies such as the Oregon Railroad and Navigation Company began to supplement steamboat operations as the major transportation links along the river. As early as 1881, industrialists proposed altering the natural channel of
17760-428: 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 Bruno de Heceta sighted the river's mouth in 1775. On May 11, 1792,
17908-498: The region. Following Hezeta's reports, British maritime fur trader Captain John Meares searched for the river in 1788 but concluded that it did not exist. He named Cape Disappointment for the non-existent river, not realizing the cape marks the northern edge of the river's mouth. What happened next would form the basis for decades of both cooperation and dispute between British and American exploration of, and ownership claim to,
18056-627: The region. Royal Navy commander George Vancouver sailed past the mouth in April 1792 and observed a change in the water's color, but he accepted Meares' report and continued on his journey northward. Later that month, Vancouver encountered the American captain Robert Gray at the Strait of Juan de Fuca . Gray reported that he had seen the entrance to the Columbia and had spent nine days trying but failing to enter. On May 12, 1792, Gray returned south and crossed
18204-717: The region. For many the final leg of the journey involved travel down the lower Columbia River to Fort Vancouver. This part of the Oregon Trail, the treacherous stretch from The Dalles to below the Cascades, could not be traversed by horses or wagons (only watercraft, at great risk). This prompted the 1846 construction of the Barlow Road . In the Treaty of 1818 the United States and Britain agreed that both nations were to enjoy equal rights in Oregon Country for 10 years. By 1828, when
18352-568: The river he had not yet seen, becoming the first Euro-descended person to travel the entire length of the river. In 1825, the Hudson's Bay Company (HBC) established Fort Vancouver on the bank of the Columbia, in what is now Vancouver, Washington, as the headquarters of the company's Columbia District , which encompassed everything west of the Rocky Mountains, north of California, and south of Russian-claimed Alaska. Chief Factor John McLoughlin ,
18500-518: The river in 1792, proved that it was possible to cross the Columbia Bar. Many of the challenges associated with that feat remain today; even with modern engineering alterations to the mouth of the river, the strong currents and shifting sandbar make it dangerous to pass between the river and the Pacific Ocean. The use of steamboats along the river, beginning with the British Beaver in 1836 and followed by American vessels in 1850, contributed to
18648-451: The river ranks 23rd in length, and the Canadian part of its basin ranks 13th in size among Canadian basins. The Columbia shares its name with nearby places, such as British Columbia, as well as with landforms and bodies of water. With an average flow at the mouth of about 265,000 cu ft/s (7,500 m /s), the Columbia is the largest river by discharge flowing into the Pacific from
18796-479: The river to break through the barrier; estimates range from several months to several years. Much of the landslide's debris remained, forcing the river about 1.5 miles (2.4 km) south of its previous channel and forming the Cascade Rapids . In 1938, the construction of Bonneville Dam inundated the rapids as well as the remaining trees that could be used to refine the estimated date of the landslide. In 1980,
18944-635: The river's upper reaches in Canada. All three terms essentially mean "the big river". Oral histories describe the formation and destruction of the Bridge of the Gods , a land bridge that connected the Oregon and Washington sides of the river in the Columbia River Gorge. The bridge, which aligns with geological records of the Bonneville Slide, was described in some stories as the result of a battle between gods, represented by Mount Adams and Mount Hood , in their competition for
19092-454: The river, but nearly all the British colonists moved south to the Willamette Valley. The hope that the British colonists might dilute the American presence in the valley failed in the face of the overwhelming number of American settlers. These developments rekindled the issue of "joint occupation" and the boundary dispute . While some British interests, especially the Hudson's Bay Company, fought for
19240-471: The sale of cheap hydropower. After a series of studies and site investigations, the dam was abandoned as a project in order to facilitate legislation creating the Central Arizona Project . The dam sites were incorporated into Marble Canyon National Monument in 1968, which was absorbed into Grand Canyon National Park in 1975. First proposed in the 1940s by the United States Bureau of Reclamation ,
19388-412: The second at 39.4 miles (63.4 km). A 25-mile (40 km) road had to be built to connect the nearest highway to "one of the most inaccessible damsites ever explored by Bureau of Reclamation engineers". In 1949 the Bureau opened bids for the construction of a 3,400-foot (1,000 m) cableway to transport workers and materials down into the remote canyon at Mile 32.8. Once the cableway was completed,
19536-430: The so-called "joint occupation" was renewed indefinitely, it seemed probable that the lower Columbia River would in time become the border between the two nations. For years the Hudson's Bay Company successfully maintained control of the Columbia River and American attempts to gain a foothold were fended off. In the 1830s, American religious missions were established at several locations in the lower Columbia River region. In
19684-457: The total watershed. Flow rates on the Columbia are affected by many large upstream reservoirs, many diversions for irrigation, and, on the lower stretches, reverse flow from the tides of the Pacific Ocean. The National Ocean Service observes water levels at six tide gauges and issues tide forecasts for twenty-two additional locations along the river between the entrance at the North Jetty and
19832-459: The tributary canyons. The retention dam in Paria Canyon was planned to be 380 feet (120 m) tall, and only 70 feet (21 m) wide at the base and 120 feet (37 m) wide at the crest, retaining 100 years of silt deposits. Despite these measures, the Marble Canyon reservoir was projected to have a lifespan of 104 years before filling with silt. One appealing aspect of a Marble Canyon damsite
19980-499: The upstream limestone would prevent the reservoir from holding water. By 1968, as part of a bargain between the Arizona delegation to Congress, which supported the Central Arizona Project , and the California delegation, which opposed the project and the dam, the Marble Canyon project was dropped from the plan. In 1969 President Lyndon B. Johnson proclaimed the establishment of Marble Canyon National Monument , effectively forestalling
20128-551: The watershed, mainly through industrial pollution and barriers to fish migration. The Columbia begins its 1,243 mi (2,000 km) journey in the southern Rocky Mountain Trench in British Columbia (BC). Columbia Lake – 2,690 ft (820 m) above sea level – and the adjoining Columbia Wetlands form the river's headwaters . The trench is a broad, deep, and long glacial valley between
20276-416: The winter of 1807–08 at Kootanae House near the source of the Columbia at present-day Invermere, BC. Over the next few years he explored much of the river and its northern tributaries. In 1811 he traveled down the Columbia to the Pacific Ocean, arriving at the mouth just after John Jacob Astor 's Pacific Fur Company had founded Astoria. On his return to the north, Thompson explored the one remaining part of
20424-524: The world are hydroelectric power stations, with some hydroelectric facilities capable of generating more than double the installed capacities of the current largest nuclear power stations . Although no official definition exists for the capacity range of large hydroelectric power stations, facilities from over a few hundred megawatts are generally considered large hydroelectric facilities. Currently, only seven facilities over 10 GW ( 10,000 MW ) are in operation worldwide, see table below. Small hydro
20572-539: The world. The classification of hydropower plants starts with two top-level categories: The classification of a plant as an SHP or LHP is primarily based on its nameplate capacity , the threshold varies by the country, but in any case a plant with the capacity of 50 MW or more is considered an LHP. As an example, for China, SHP power is below 25 MW, for India - below 15 MW, most of Europe - below 10 MW. The SHP and LHP categories are further subdivided into many subcategories that are not mutually exclusive. For example,
20720-559: Was 1,240,000 cu ft/s (35,000 m /s) in June 1894, before the river was dammed. The lowest flow recorded at The Dalles was 12,100 cu ft/s (340 m /s) on April 16, 1968, and was caused by the initial closure of the John Day Dam , 28 mi (45 km) upstream. The Dalles is about 190 mi (310 km) from the mouth; the river at this point drains about 237,000 sq mi (610,000 km ) or about 91 percent of
20868-470: Was Grays Bay at the mouth of Grays River . Gray's discovery of the Columbia River was later used by the United States to support its claim to the Oregon Country, which was also claimed by Russia , Great Britain , Spain and other nations. In October 1792, Vancouver sent Lieutenant William Robert Broughton , his second-in-command, up the river. Broughton got as far as the Sandy River at the western end of
21016-573: Was allowed to provide irrigation and power to citizens (in addition to aluminium power) after the war. In Suriname , the Brokopondo Reservoir was constructed to provide electricity for the Alcoa aluminium industry. New Zealand 's Manapouri Power Station was constructed to supply electricity to the aluminium smelter at Tiwai Point . Since hydroelectric dams do not use fuel, power generation does not produce carbon dioxide . While carbon dioxide
21164-521: Was completed in 1975. Among the main commodities are wheat and other grains, mainly for export. As of 2016, the Columbia ranked third, behind the Mississippi and Paraná rivers, among the world's largest export corridors for grain. The 1980 eruption of Mount St. Helens caused mudslides in the area, which reduced the Columbia's depth by 25 feet (7.6 m) for a 4-mile (6.4 km) stretch, disrupting Portland's economy. Efforts to maintain and improve
21312-605: Was entitled to possess and/or study the remains. Many different Native Americans and First Nations peoples have a historical and continuing presence on the Columbia. South of the Canada–US ;border, the Colville , Spokane , Coeur d'Alene , Yakama , Nez Perce , Cayuse , Palus , Umatilla , Cowlitz , and the Confederated Tribes of Warm Springs live along the US stretch. Along the upper Snake River and Salmon River ,
21460-624: Was first explored in the 1920s by the United States Geological Survey , which designated sites for "an unbroken string of [hydroelectric] dams from the mountains of Colorado and Wyoming to the last canyons of the Colorado River along the California/Arizona border". Although the Bureau of Reclamation expressed interest at this time in developing hydroelectric generation at the Marble site, these plans were postponed in favor of building
21608-472: Was submerged by the construction of The Dalles Dam, and the native fishing community was displaced. The affected tribes received a $ 26.8 million settlement for the loss of Celilo and other fishing sites submerged by The Dalles Dam. The Confederated Tribes of Warm Springs used part of its $ 4 million settlement to establish the Kah-Nee-Ta resort south of Mount Hood. In 1977, 75 indigenous fishermen of
21756-530: Was the potential to develop the Grand Canyon 's hydroelectric potential without building a dam or reservoir in Grand Canyon National Park , by diverting about 90% of the Colorado River's waters at Marble Canyon into a 38-mile (61 km) tunnel, 36 feet (11 m) in diameter and capable of carrying about 14,000 cubic feet per second (400 m/s), to a site in the western part of the canyon in what
21904-535: Was then Kaibab National Forest . The plan would provide about 1,300 feet (400 m) of hydraulic head for power generation. The power plant would produce about 6.5 billion kilowatt hours (KWh) per year – almost twice that of Hoover Dam . The tunnel would allow the hydroelectric system to effectively bypass Grand Canyon National Park , avoiding the construction of more dams within the park between Marble and Bridge. A flow of 1,000 cubic feet per second (28 m/s) would be released from Marble Canyon at all times –
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