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119-637: The crossing of the Crooked River played a critical role in the competition to build a railroad up the Deschutes River Valley. The incentive for railroad construction was reaching the vast stands of timber south of Bend. The Oregon Trunk Railway Company, a subsidiary of the Spokane, Portland and Seattle Railway owned by James J. Hill of the Great Northern Railway , started up the west side of

238-582: A Union Pacific subsidiary, was owned by Edward H. Harriman and the Oregon Trunk was owned by James J. Hill . In 1964, on the Deschutes River, Portland General Electric (PGE) built, what was at the time, the largest hydroelectric dam in Oregon. This dam, named Round Butte Dam , stands 440 feet (130 m) above Lake Simtustus, a 611-acre (247 ha) reservoir impounded by Pelton Dam . The river

357-417: A big, powerful river. The average catch for these fish is 8 to 15 inches (20 to 38 cm), and some are much larger. These redside or redband trouts are found throughout the river. Fishing for them is most popular from Warm Springs down to Macks Canyon (Warm Springs Reservation owns the entire Deschutes west bank from 16 miles (26 km) south of Maupin to Lake Billy Chinook and on up to Jefferson Creek on

476-623: 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

595-564: 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

714-740: A gorge well below the surrounding countryside. It passes through the Warm Springs Indian Reservation , which includes the city of Warm Springs and the Kah-Nee-Ta resort. The river ends at its confluence with the Columbia River , 5 miles (8 km) southwest of Biggs Junction and 204 miles (328 km) from the Columbia's mouth on the Pacific Ocean. Named tributaries of the Deschutes River from source to mouth include Snow Creek then

833-578: 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

952-520: 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,

1071-681: 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

1190-471: 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

1309-533: 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

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1428-661: 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

1547-518: 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

1666-599: 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

1785-537: Is world-renowned for its fly fishing . It is home to Columbia River redband trout ( Oncorhynchus mykiss gairdneri ) known locally as "redsides". The redsides grow larger than most and also have a distinct darker red stripe than most wild rainbow trout. They are abundant in this stretch of the river, which has counts of 1,700 fish of 7 inches in size per mile (1,100 fish of 18 centimeters in size per kilometer) above Sherar's Falls , and they are noticeably stronger than trout who do not have to cope with life in such

1904-871: 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

2023-646: 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

2142-487: The Cascade Range in Oregon, gathering many of the tributaries that descend from the drier, eastern flank of the mountains. The Deschutes provided an important route to and from the Columbia for Native Americans for thousands of years, and then in the 19th century for pioneers on the Oregon Trail . The river flows mostly through rugged and arid country, and its valley provides a cultural heart for central Oregon. Today

2261-547: 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

2380-576: 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 ),

2499-675: The Cultus River , Cultus Creek and Deer Creek, which enter at Crane Prairie Reservoir. Further downstream come the Fall River , the Little Deschutes River , and the Spring River followed by Tumalo Creek and Whychus Creek . The Metolius River and the Crooked River are next, both entering at Lake Billy Chinook. Then come Seekseequa Creek and Willow Creek followed by Dry Hollow and Campbell, Shitike and Trout creeks, after which comes

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2618-702: 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

2737-581: 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

2856-607: 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

2975-556: The Metolius River arm) below Pelton Dam . Fishing from Tribal lands requires special permits. From Pelton Dam to the mouth the Deschutes is one of America's most productive trout waters and a top producer of summer steelhead, managed primarily for wild trout. This 100-mile (160 km) stretch of river drops 1,233 feet (376 m), carving a volcanic rock canyon 700 to 2,200 feet (213 to 671 m) deep. Fly fishermen come from around

3094-600: 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

3213-548: 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

3332-517: 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

3451-467: The Oregon Trail . The major crossing point on the river was near its mouth in present-day Deschutes River State Recreation Area . Many immigrants camped on the bluff on the west side of the river after making the crossing. The remains of the trail leading up to the top of the bluff are still visible. In 1910, Mirror Pond was created by the construction of the Bend Water, Light & Power Company dam on

3570-763: 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

3689-523: The Warm Springs River . Further downstream are Swamp, Skookum, Oak, Antoken, Cove, Eagle, Nena, Wapinitia and Bakeoven creeks. Spring Creek is next, followed by Oak Springs Creek and the White River . Below that are Winterwater and Elder creeks. Prior to 80,000 years ago, the river ran along the east side of Pilot Butte and a lava flow from Lava Top Butte filled in this ancient channel. Previously,

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3808-473: 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

3927-455: 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

4046-534: 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

4165-452: 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

4284-473: 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

4403-460: 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,

4522-594: 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

4641-489: 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

4760-486: 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

4879-538: 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;

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4998-417: 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,

5117-478: 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

5236-734: 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

5355-466: 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

5474-463: 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

5593-406: 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

5712-481: 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

5831-406: 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

5950-409: The Deschutes while the Des Chutes Railroad, owned by Edward Harriman of the Union Pacific , started up the east side. At North Junction, approximately 65 miles (105 km) south of the Columbia River, Hill's Oregon Trunk crossed over to the east bank. At 126 miles (203 km) both railroads would have had to cross a major tributary of the Deschutes, the Crooked River. There was only one place where

6069-499: The Galveston Bridge and is a feature of Drake Park as well as Harmon, Pageant, and Brooks parks. From April through October, diversions to Central Oregon Irrigation District canals reduce the river flow between Bend and Pelton Reregulating Dam , at river mile (RM) 100 (river kilometer (RK) 160). The river continues north from Bend, and just west of Redmond, Oregon . Here it passes by Eagle Crest Resort and Cline Falls State Scenic Viewpoint . As it heads north through

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6188-402: 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

6307-411: 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

6426-418: 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

6545-421: 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

6664-407: 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

6783-491: 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

6902-449: 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

7021-540: 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

7140-448: The basalt of the Bend lava flow, associated with the Lava River Cave , had diverted the river westward to its present-day location. The river was named Rivière des Chutes or Rivière aux Chutes , French for River of the Falls , during the period of fur trading. The waterfall it referred to was the Celilo Falls on the Columbia River , near where the Deschutes flowed into it. (These falls no longer exist, having been inundated by

7259-412: 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

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7378-420: The bridge's construction were taken by Olof Hedlund of Madras. Less than 1 ⁄ 4 mile (0.40 km) upriver from the bridge are the Crooked River High Bridge , the Rex T. Barber Veterans Memorial Bridge (which carries U.S. Route 97 over the Crooked River), and the Peter Skene Ogden State Scenic Viewpoint . Further upriver the City of Prineville Railway , linking Redmond and Prineville , operates

7497-460: 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

7616-426: The central Oregon high desert , the river carves a gorge bordered by large basalt cliffs. By the time it reaches Lake Billy Chinook , a reservoir west of Madras , the river is approximately 300 feet (91 m) below the surrounding plateau, the Little Agency Plains and Agency Plains . At Lake Billy Chinook the river is joined by the Crooked and Metolius rivers. Beyond the dam, the river continues north in

7735-477: The channels can be wide and deep. Located roughly seven miles southeast of Crane Prairie Reservoir, you will find Wickiup Reservoir. Wickiup Reservoir holds a wide variety of species open to angling. Wickiup holds a reputable amount of both kokanee and Coho salmon . It is not uncommon to catch rainbow trout, brook trout, whitefish and chub. However, most anglers whether they know it or not, are targeting large brown trout. Wickiup Reservoir holds many brown trout in

7854-428: The city of La Pine . The river flows south into Crane Prairie Reservoir , then into Wickiup Reservoir , from where it heads in a northeasterly direction past the resort community of Sunriver and into the city of Bend , about 170 miles (270 km) from the river mouth on the Columbia. In central Bend, the river enters Mirror Pond , an impoundment behind Newport hydroelectric dam . The pond extends upstream to

7973-441: The cliffs on both sides were close enough to build a bridge. Jim Hill had obtained the rights to the location when his Oregon Trunk Railroad acquired the Central Oregon Railroad Company on December 1, 1909. The Central Oregon had laid no track and the rights to the bridge site were its principal asset. Hill's acquisition of the location forced Harriman to negotiate a settlement whereby the Oregon Trunk, Hill's railroad, would own almost

8092-419: 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

8211-410: 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

8330-449: 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

8449-405: The crew lived two miles north of the bridge in a large construction camp at Opal City. Opal City was expected to thrive well into the future but it was completely abandoned soon after the railroad was completed. The first steel for the bridge arrived on May 18, 1911, and was lowered by derrick to the bottom of the gorge. Men climbed down rope ladders to attach cables to the steel beams and the steel

8568-468: 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

8687-496: The entire line from the Columbia to Bend but Harriman's company would have the right to use the track. Through a series of mergers the rail line and the bridge became part of the Burlington Northern and Santa Fe Railway (which changed its name to BNSF Railway in 2005). Union Pacific, Harriman's old railroad, still has the right to use the track. Great Northern extended the line south from Bend to Chemult in 1928. The bridge

8806-477: The five to eight pound range, and has also been known to produce brown trout in the mid-twenty pound range. This reservoir is most easily fished from a boat due to its depth. Most people find success in trolling lures horizontally through the depths of the reservoir. Vertical jigging in an aggressive manner can be an effective method of targeting the salmon species of the reservoir. Bank fishing offers dry fly-fishing enthusiasts an opportunity to catch fish hiding under

8925-452: 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

9044-427: 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

9163-518: 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

9282-535: The lake behind The Dalles Dam ). Lewis and Clark encountered the river on October 22, 1805, and referred to it by the Native American name Towarnehiooks ; on their return journey they gave it the new name Clarks River . Variant names include Clarks River, River of the Falls, Riviere des Chutes, Chutes River, and Falls River. During the middle 19th century, the river was a major obstacle for immigrants on

9401-447: 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

9520-442: 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

9639-577: 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

9758-464: 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

9877-466: The nickname "cranebows". Other fish found in Crane Prairie are brook trout , kokanee salmon , largemouth bass , black crappie , tui chub , three-spined stickleback , and whitefish . Fly, lure, and bait fishing are popular methods, with the majority of trout fisherman casting or trolling in the channels. For the best chance of catching large fish, a boat or other flotation device is recommended as

9996-580: 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 ,

10115-400: The obstructions of the shallows. In Lake Billy Chinook, there are fisheries for kokanee , bull trout , rainbow trout , brown trout , and several warm-water species such as large mouth bass and a very large population of small mouth bass. There are also periodic commercial fisheries for crayfish . The bull trout that are caught in this reservoir are some of the largest bull trout caught on

10234-407: The only other railroad bridge across the Crooked River. 44°23′28″N 121°11′46″W  /  44.3911°N 121.1962°W  / 44.3911; -121.1962 Deschutes River, Oregon The Deschutes River ( / d ə ˈ ʃ uː t s / də- SHOOTS ) in central Oregon is a major tributary of the Columbia River . The river provides much of the drainage on the eastern side of

10353-467: 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

10472-532: 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

10591-688: 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,

10710-735: 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

10829-460: 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

10948-428: 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,

11067-498: 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,

11186-627: 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

11305-717: 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

11424-482: The river from the mouth to Round Butte Dam . Sport fishing for spring and fall Chinook salmon occurs from the mouth to Sherars Falls. Tribal fishing for Chinook and steelhead occurs at Sherars Falls. Crane Prairie Reservoir, the first major lake/reservoir the Deschutes flows into, offers some of the best rainbow trout fishing in Oregon, with a large number of rainbows in the 4-10 pound range and some reaching 20 pounds. These trout are renowned for their size and are given

11543-568: 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 ,

11662-571: The river in Bend . The dam provided the city with its initial source of electricity. The dam has been owned by Pacific Power since 1930 and still produces electricity that supplies approximately 400 Bend households. In 1908, two competing railroad companies, the Deschutes Railroad and the Oregon Trunk Railway , raced to build a line from the mouth of the river to Bend. The Deschutes Railroad,

11781-518: 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

11900-660: The river popular for whitewater rafting and kayaking. The upstream section known as the Big Eddy is a short segment upriver from the city of Bend between Dillon and Lava Island falls. The lower and more heavily used section is from the town of Warm Springs downstream to just above Sherars Falls . The densest use is from RM 56—about 4 miles (6.4 km) above Maupin —to RM 44, just above Sherars Falls. Columbia River The Columbia River ( Upper Chinook : Wimahl or Wimal ; Sahaptin : Nch’i-Wàna or Nchi wana ; Sinixt dialect swah'netk'qhu )

12019-451: 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

12138-468: The river supplies water for irrigation and is popular in the summer for whitewater rafting and fishing . The Deschutes flows generally north, as do several other large Oregon tributaries of the Columbia River, including the Willamette and John Day . The headwaters of the Deschutes River are at Little Lava Lake , a natural lake in the Cascade Range approximately 26 miles (42 km) northwest of

12257-479: 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,

12376-525: The river's flow in the summer months. The growth of cities like Bend and Redmond also increased demand on the river's water, which is over-allocated. Because the existing canals lose about half of their water due to seepage, there is pressure to convert these canals into pipelines, a move that is resisted by many locals for historic and aesthetic reasons. Golf courses have also been an issue with water allocation. There are 13 golf courses throughout Bend, Redmond, and Sunriver. There are primarily two sections of

12495-635: 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

12614-454: 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

12733-430: 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

12852-457: 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

12971-551: 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

13090-418: The west coast. The numbers are scarce because the bulls are threatened; however, numbers have risen every year since they became protected. The lake allows an individual to keep a bull trout that measures more than 24 inches (61 cm). (This is included for a daily bag limit.) Much of the flow of the upper Deschutes River is diverted into canals to irrigate farmland; irrigation districts take nearly 98% of

13209-416: 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

13328-534: The world in the last two weeks in May through the first two weeks in June to take advantage of the hatching stoneflies , both salmonflies and golden stoneflies ( Hesperoperla pacifica ). These insects are in the river year-round; however their large adults are a major food source for the fish: artificial weighted stonefly nymph patterned tied flies are a staple for Deschutes anglers year round. Sport fishing for Steelhead occurs in

13447-512: 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

13566-470: 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

13685-521: 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

13804-517: Was designed by the famous bridge architect, Ralph Modjeski , who also designed the San Francisco–Oakland Bay Bridge . The Missouri Valley Bridge & Iron Company built the bridge by cantilevering it out from rock walls on both sides of the canyon. A myth arose, fostered by a photograph of men climbing a rope ladder up to the bridge, that the bridge builders camped at the bottom of the canyon and climbed up to work every day. In fact

13923-605: 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 ,

14042-431: Was hoisted back up both sides of the canyon as the beams were needed. The first train crossed the bridge only four months later on September 17. Half the rivets holding the bridge together were installed after trains started using the bridge. The bridge was built quickly to facilitate laying the last 25.5 miles (41.0 km) of track to Bend where Jim Hill himself drove the "golden" spike on October 5. Dramatic photographs of

14161-420: 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

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