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Fraser River

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Fraser River
Staulo,[1] Lhtako,[2] Tacoutche Tesse,[3] ʔElhdaqox,[4] Sto:lo
FraserRiver.jpg
The Fraser River, from the grounds of Westminster Abbey, above Hatzic in Mission, British Columbia, looking upstream (E)
Fraser River Watershed.png
Fraser River watershed
Fraser River is located in British Columbia
Fraser River
Location of mouth
EtymologyFur trader and explorer Simon Fraser
Location
CountryCanada
ProvinceBritish Columbia
Regional districts
Cities
Physical characteristics
SourceFraser Pass
 • locationMount Robson Provincial Park, Rocky Mountains, British Columbia, Canada
 • coordinates52°37′41″N 118°25′50″W / 52.62806°N 118.43056°W / 52.62806; -118.43056
 • elevation2,145 m (7,037 ft)
MouthFraser River Delta
 • location
Strait of Georgia, Vancouver, British Columbia, Canada
 • coordinates
49°10′40″N 123°12′45″W / 49.17778°N 123.21250°W / 49.17778; -123.21250Coordinates: 49°10′40″N 123°12′45″W / 49.17778°N 123.21250°W / 49.17778; -123.21250
 • elevation
0 m (0 ft)
Length1,375 km (854 mi)[5]
Basin size220,000 km2 (85,000 sq mi)
Discharge 
 • locationmouth (average and min); max at Hope[6][7]
 • average3,475 m3/s (122,700 cu ft/s)
 • minimum575 m3/s (20,300 cu ft/s)
 • maximum17,000 m3/s (600,000 cu ft/s)
Basin features
Tributaries 
 • leftBowron River, Willow River, Quesnel River, Thompson River, Coquihalla River, Chilliwack River, Sumas River, Salmon River (lower mainland)
 • rightMorkill River, McGregor River, Salmon River (interior), Nechako River, West Road (Blackwater) River, Chilcotin River, Bridge River, Harrison River, Stave River, Pitt River, Coquitlam River
Protection status
Official nameFraser River Delta
Designated24 May 1982
Reference no.243[8]

The Fraser River /ˈfrzər/ is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for 1,375 kilometres (854 mi), into the Strait of Georgia just south of the City of Vancouver.[5][9] The river's annual discharge at its mouth is 112 cubic kilometres (27 cu mi) or 3,550 cubic metres per second (125,000 cu ft/s), and it discharges 20 million tons of sediment into the ocean.[10]

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British Columbia

British Columbia

British Columbia, commonly abbreviated as BC, is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east, the territories of Yukon and Northwest Territories to the north, and the US states of Washington, Idaho and Montana to the south and Alaska to the northwest. With an estimated population of 5.3 million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6 million people in Metro Vancouver.

Fraser Pass

Fraser Pass

The Fraser Pass is a mountain pass in the British Columbian Rockies of Western Canada. Its summit is 2,015 m (6,611 ft) above sea level. Although immediately adjacent to the Continental Divide, the pass does not cross it; rather, it bridges the drainage basins of the Fraser River and Columbia River, both Pacific-draining rivers.

Blackrock Mountain (Canada)

Blackrock Mountain (Canada)

Blackrock Mountain is located on the border of Alberta and British Columbia. It was named in 1921 by Arthur O. Wheeler for the black Ordovician rock present in the area.

Rocky Mountains

Rocky Mountains

The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 miles in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west.

Strait of Georgia

Strait of Georgia

The Strait of Georgia or the Georgia Strait is an arm of the Salish Sea between Vancouver Island and the extreme southwestern mainland coast of British Columbia, Canada and the extreme northwestern mainland coast of Washington, United States. It is approximately 240 kilometres (150 mi) long and varies in width from 20 to 58 kilometres. Along with the Strait of Juan de Fuca and Puget Sound, it is a constituent part of the Salish Sea.

Naming

The river is named after Simon Fraser, who led an expedition in 1808 on behalf of the North West Company from the site of present-day Prince George almost to the mouth of the river. The river's name in the Halqemeylem (Upriver Halkomelem) language is Sto:lo, often seen archaically as Staulo, and has been adopted by the Halkomelem-speaking peoples of the Lower Mainland as their collective name, Sto:lo. The river's name in the Dakelh language is Lhtakoh.[11] The Tsilhqot'in name for the river, not dissimilar to the Dakelh name, is ʔElhdaqox, meaning Sturgeon (ʔElhda-chugh) River (Yeqox).

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Simon Fraser (explorer)

Simon Fraser (explorer)

Simon Fraser was a Canadian explorer and fur trader who charted much of what is now the Canadian province of British Columbia. He also built the first European settlement in British Columbia.

North West Company

North West Company

The North West Company was a fur trading business headquartered in Montreal from 1779 to 1821. It competed with increasing success against the Hudson's Bay Company in what is present-day Western Canada and Northwestern Ontario. With great wealth at stake, tensions between the companies increased to the point where several minor armed skirmishes broke out, and the two companies were forced by the British government to merge.

Prince George, British Columbia

Prince George, British Columbia

Prince George is a city in British Columbia, Canada, with a city population of 76,708 and a metro census agglomeration population of 89,490. It is often called the province's "northern capital". It is situated at the confluence of the Fraser and Nechako rivers.

Sturgeon

Sturgeon

Sturgeon is the common name for the 27 species of fish belonging to the family Acipenseridae. The earliest sturgeon fossils date to the Late Cretaceous, and are descended from other, earlier acipenseriform fish, which date back to the Early Jurassic period, some 174 to 201 million years ago. They are one of two living families of the Acipenseriformes alongside paddlefish (Polyodontidae). The family is grouped into four genera: Acipenser, Huso, Scaphirhynchus, and Pseudoscaphirhynchus. Two species may be extinct in the wild, and one may be entirely extinct. Sturgeons are native to subtropical, temperate and sub-Arctic rivers, lakes and coastlines of Eurasia and North America.

Course

Fraser River drainage basin
Fraser River drainage basin

The Fraser drains a 220,000-square-kilometre (85,000 sq mi) area. Its source is a dripping spring at Fraser Pass in the Canadian Rocky Mountains near the border with Alberta. The river then flows north to the Yellowhead Highway and west past Mount Robson to the Rocky Mountain Trench and the Robson Valley near Valemount. After running northwest past 54° north, it makes a sharp turn to the south at Giscome Portage, meeting the Nechako River at the city of Prince George, then continues south, progressively cutting deeper into the Fraser Plateau to form the Fraser Canyon from roughly the confluence of the Chilcotin River, near the city of Williams Lake, southwards. It is joined by the Bridge and Seton Rivers at the town of Lillooet, then by the Thompson River at Lytton, where it proceeds south until it is approximately 64 kilometres (40 mi) north of the 49th parallel, which is Canada's border with the United States.

From Lytton southwards it runs through a progressively deeper canyon between the Lillooet Ranges of the Coast Mountains on its west and the Cascade Range on its east. Hell's Gate, located immediately downstream of the town of Boston Bar, is a famous portion of the canyon where the walls narrow dramatically, forcing the entire volume of the river through a gap only 35 metres (115 feet) wide. An aerial tramway takes visitors out over the river. Hells Gate is visible from Trans-Canada Highway 1 about 2 km (1.2 mi) south of the tramway. Simon Fraser was forced to portage the gorge on his trip through the canyon in June 1808.

At Yale, at the head of navigation on the river, the canyon opens up and the river widens, though without much adjoining lowland until Hope, where the river then turns west and southwest into the Fraser Valley, a lush lowland valley, and runs past Chilliwack and the confluence of the Harrison and Sumas Rivers, bending northwest at Abbotsford and Mission.

The Fraser then flows past Maple Ridge, Pitt Meadows, Port Coquitlam, and north Surrey. It turns southwest again just east of New Westminster, where it splits into the North Arm,[12] which is the southern boundary of the City of Vancouver, and the South Arm, which divides the City of Richmond from the City of Delta to the south. Richmond is on the largest island in the Fraser, Lulu Island and also on Sea Island, which is the location of Vancouver International Airport, where the Middle Arm branches off to the south from the North Arm. The far eastern end of Lulu Island is named Queensborough and is part of the City of New Westminster. Also in the lowermost Fraser, among other smaller islands, is Annacis Island, an important industrial and port area, which lies to the southeast of the eastern end of Lulu Island. Other notable islands in the lower Fraser are Barnston Island, Matsqui Island, Nicomen Island and Sea Bird Island. Other islands lie on the outer side of the estuary, most notably Westham Island, a wildfowl preserve, and Iona Island, the location of the main sewage plant for the City of Vancouver.

After 100 kilometres (about 60 mi), the Fraser forms a delta where it empties into the Strait of Georgia between the mainland and Vancouver Island. The lands south of the City of Vancouver, including the cities of Richmond and Delta, sit on the flat flood plain. The islands of the delta include Iona Island, Sea Island, Lulu Island, Annacis Island, and a number of smaller islands. While the vast majority of the river's drainage basin lies within British Columbia, a small portion in the drainage basin lies across the international border in Washington in the United States, namely the upper reaches of the tributary Chilliwack and Sumas rivers. Most of lowland Whatcom County, Washington is part of the Fraser Lowland and was formed also by sediment deposited from the Fraser, though most of the county is not in the Fraser drainage basin.

Similar to the Columbia River Gorge east of Portland, Oregon, the Fraser exploits a topographic cleft between two mountain ranges separating a more continental climate (in this case, that of the British Columbia Interior) from a milder climate near the coast. When an Arctic high-pressure area moves into the British Columbia Interior and a relatively low-pressure area builds over the general Puget Sound and Strait of Georgia region, the cold Arctic air accelerates southwest through the Fraser Canyon. These outflow winds can gust up to 97 to 129 kilometres per hour (60 to 80 mph) and have at times exceeded 160 kilometres per hour (100 mph). Such winds frequently reach Bellingham and the San Juan Islands, gaining strength over the open water of the Strait of Juan de Fuca.[13]

The estuary at the river's mouth is a site of hemispheric importance in the Western Hemisphere Shorebird Reserve Network.[14]

Discharge

The Water Survey of Canada currently operates 17 gauge stations that measure discharge and water level along the majority of the mainstem from Red Pass just downstream of Moose Lake in the Mount Robson Provincial Park, to Steveston in Vancouver at the river mouth.[15] With an average flow at the mouth of about 3,475 cubic metres per second (122,700 cu ft/s),[16] the Fraser is the largest river by discharge flowing into the Pacific seaboard of Canada and the fifth largest in the country.[17] The average flow is highly seasonal; summer discharge rates can be ten times larger than the flow during the winter.[17]

The Fraser's highest recorded flow, in June 1894, is estimated to have been 17,000 cubic metres per second (600,000 cu ft/s) at Hope. It was calculated using high-water marks near the hydrometric station at Hope and various statistical methods. In 1948 the Fraser River Board adopted the estimate for the 1894 flood. It remains the value specified by regulatory agencies for all flood control work on the river.[7] Further studies and hydraulic models have estimated the maximum discharge of the Fraser River, at Hope during the 1894 flood, as within a range of about 16,000 to 18,000 cubic metres per second (570,000 to 640,000 cu ft/s).[7]

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Fraser Pass

Fraser Pass

The Fraser Pass is a mountain pass in the British Columbian Rockies of Western Canada. Its summit is 2,015 m (6,611 ft) above sea level. Although immediately adjacent to the Continental Divide, the pass does not cross it; rather, it bridges the drainage basins of the Fraser River and Columbia River, both Pacific-draining rivers.

Canadian Rockies

Canadian Rockies

The Canadian Rockies or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.

Alberta

Alberta

Alberta is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada. The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds.

Mount Robson

Mount Robson

Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.

Giscome Portage

Giscome Portage

The Giscome Portage was a portage between the Fraser River and Summit Lake, which connected with the river route to the Peace Country via Finlay Forks. BC Parks administers the Giscome Portage Trail. The Huble Homestead Historic Site, at the south end, is on the Fraser River, 40 kilometres (25 mi) north of Prince George and 6 kilometres (3.7 mi) off Highway 97.

Nechako River

Nechako River

The Nechako River arises on the Nechako Plateau east of the Kitimat Ranges of the Coast Mountains of British Columbia, Canada, and flows north toward Fort Fraser, then east to Prince George where it enters the Fraser River. "Nechako" is an anglicization of netʃa koh, its name in the indigenous Carrier language which means "big river".

Fraser Plateau

Fraser Plateau

The Fraser Plateau is an intermontane plateau. It is one of the main subdivisions of the Interior Plateau located in the Central Interior of British Columbia.

Fraser Canyon

Fraser Canyon

The Fraser Canyon is a major landform of the Fraser River where it descends rapidly through narrow rock gorges in the Coast Mountains en route from the Interior Plateau of British Columbia to the Fraser Valley. Colloquially, the term "Fraser Canyon" is often used to include the Thompson Canyon from Lytton to Ashcroft, since they form the same highway route which most people are familiar with, although it is actually reckoned to begin above Williams Lake, British Columbia at Soda Creek Canyon near the town of the same name.

Chilcotin River

Chilcotin River

The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This 19,200 km2 (7,400 sq mi) watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, 22 km (14 mi) upstream from Gang Ranch.

Bridge River

Bridge River

The Bridge River is an approximately 120 kilometres (75 mi) long river in southern British Columbia. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of Lillooet; its flow, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project, with the water now entering the Fraser just south of Lillooet as a result.

Lillooet

Lillooet

Lillooet is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road about 100 kilometres (62 mi) northeast of Pemberton, 64 kilometres (40 mi) northwest of Lytton, and 172 kilometres (107 mi) west of Kamloops.

Lytton, British Columbia

Lytton, British Columbia

Lytton is a village of about 250 residents in southern British Columbia, Canada, on the east side of the Fraser River and primarily the south side of the Thompson River, where it flows southwesterly into the Fraser. The community includes the Village of Lytton and the surrounding community of the Lytton First Nation, whose name for the place is Camchin, also spelled Kumsheen.

History

The Descent of the Fraser River, 1808, by C.W. Jefferys
The Descent of the Fraser River, 1808, by C.W. Jefferys
Fraser River in Lillooet
Fraser River in Lillooet
Source of Fraser River at Fraser Pass
Source of Fraser River at Fraser Pass

On June 14, 1792, the Spanish explorers Dionisio Alcalá Galiano and Cayetano Valdés entered and anchored in the North Arm of the Fraser River, becoming the first Europeans to find and enter it.[18] The existence of the river, but not its location, had been deduced during the 1791 voyage of José María Narváez, under Francisco de Eliza.

The upper reaches of the Fraser River were first explored by Sir Alexander Mackenzie in 1793, and fully traced by Simon Fraser in 1808, who confirmed that it was not connected with the Columbia River.

The lower Fraser was revisited in 1824 when the Hudson Bay Company sent a crew across Pudget Sound from its Fort George southern post located on the Columbia River. The expedition was led by James McMillan. The Fraser was reached via the Nicomekl River and the Salmon River reachable after a portage. Friendly tribes met earlier on by the Simon Fraser crew were reacquainted with. A trading post with agricultural potential was to be located.

By 1827, a crew was sent back via the mouth of the Fraser to build and operate the original Fort Langley.[19] McMillan also led the undertaking. The trading post original location would soon become the first ever mixed ancestry and agricultural settlement in southern British Columbia on the Fraser (Sto:lo) river.[20]

In 1828 George Simpson visited the river, mainly to examine Fort Langley and determine whether it would be suitable as the Hudson's Bay Company's main Pacific depot. Simpson had believed the Fraser River might be navigable throughout its length, even though Simon Fraser had described it as non-navigable. Simpson journeyed down the river and through the Fraser Canyon and afterwards wrote "I should consider the passage down, to be certain Death, in nine attempts out of Ten. I shall therefore no longer talk about it as a navigable stream". His trip down the river convinced him that Fort Langley could not replace Fort Vancouver as the company's main depot on the Pacific coast.[21]

Much of British Columbia's history has been bound to the Fraser, partly because it was the essential route between the Interior and the Lower Coast after the loss of the lands south of the 49th Parallel with the Oregon Treaty of 1846.[22] It was the site of its first recorded settlements of Aboriginal people (see Musqueam, Sto:lo, St'at'imc, Secwepemc and Nlaka'pamŭ), the site of the first European-Indigenous mixed ancestry settlement in southern British-Columbia (see Fort Langley), the route of multitudes of prospectors during the Fraser Canyon Gold Rush and the main vehicle of the province's early commerce and industry.

In 1998, the river was designated as a Canadian Heritage River for its natural and human heritage. It remains the longest river with that designation.[5]

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Dionisio Alcalá Galiano

Dionisio Alcalá Galiano

Dionisio Alcalá Galiano was a Spanish naval officer, cartographer, and explorer. He mapped various coastlines in Europe and the Americas with unprecedented accuracy using new technology such as chronometers. He commanded an expedition that explored and mapped the Strait of Juan de Fuca and the Strait of Georgia, and made the first European circumnavigation of Vancouver Island. He reached the rank of brigadier and died during the Battle of Trafalgar.

Cayetano Valdés y Flores

Cayetano Valdés y Flores

Cayetano Valdés y Flores Bazán (1767–1835) was a commander of the Spanish Navy, explorer, and captain general who served in the French Revolutionary and Napoleonic Wars, fighting for both sides at different times due to the changing fortunes of Spain in the conflict. He took part in a number of naval battles, including the Great Siege of Gibraltar, the Battle of Cape St Vincent, and the Battle of Trafalgar. He was an explorer, most notable in the Pacific Northwest, where he and Dionisio Alcalá Galiano conducted the first circumnavigation of Vancouver Island, in partial cooperation with George Vancouver. Over his long career he achieved the highest ranks in the Spanish Navy, eventually being named Captain General of Cadiz and Captain General of the Spanish Navy.

José María Narváez

José María Narváez

José María Narváez was a Spanish naval officer, explorer, and navigator notable for his work in the Gulf Islands and Lower Mainland of present-day British Columbia. In 1791, as commander of the schooner Santa Saturnina, he led the first European exploration of the Strait of Georgia, including a landing on present-day British Columbia's Sunshine Coast. He also entered Burrard Inlet, the site of present-day Vancouver, British Columbia.

Francisco de Eliza

Francisco de Eliza

Francisco de Eliza y Reventa was a Spanish naval officer, navigator, and explorer. He is remembered mainly for his work in the Pacific Northwest. He was the commandant of the Spanish post in Nootka Sound on Vancouver Island, and led or dispatched several exploration voyages in the region, including the Strait of Juan de Fuca and the Strait of Georgia.

Columbia River

Columbia River

The Columbia River is a major river which flows through southern British Columbia, central Washington and forms a portion of the Washington - Oregon boundary before emptying into the Pacific Ocean. It is the largest river in the Pacific Northwest region of the United States. The river rises 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 miles long, and its largest tributary is the Snake River. Its drainage basin is roughly the size of France and extends into seven of the United States plus a Canadian province. The fourth-largest river in the United States by volume, the Columbia has the greatest flow of any North American river entering the Pacific. The Columbia has the 36th greatest discharge of any river in the world.

Fort Astoria

Fort Astoria

Fort Astoria was the primary fur trading post of John Jacob Astor's Pacific Fur Company (PFC). A maritime contingent of PFC staff was sent on board the Tonquin, while another party traveled overland from St. Louis. This land based group later became known as the Astor Expedition. Built at the entrance of the Columbia River in 1811, Fort Astoria was the first American-owned settlement on the Pacific coast of North America.

James McMillan (fur trader)

James McMillan (fur trader)

James McMillan was a fur trader and explorer for the North West Company and Hudson's Bay Company. He led some of the earliest surveys of the lower Fraser River and founded Fort Langley for the HBC in 1827, and was its first Chief Trader.

Nicomekl River

Nicomekl River

The Nicomekl River springs from the ground in Langley, British Columbia and travels west through the city to Surrey's Crescent Beach, where it empties into Mud Bay, the northernmost section of the Boundary Bay of the Strait of Georgia. It has a total length of 34 km, with a drainage area of 149 km2.

Salmon River (Langley)

Salmon River (Langley)

The Salmon River is a small river in the Township of Langley in the Lower Mainland region of British Columbia, Canada, flowing northwest then northeast to enter Bedford Channel, which separates McMillan Island from Fort Langley, which is just southwest.

Fort Langley National Historic Site

Fort Langley National Historic Site

Fort Langley National Historic Site, commonly shortened to Fort Langley, is a former fur trading post of the Hudson's Bay Company in the community of Fort Langley of Langley, British Columbia, Canada. The national historic site sits above the banks of the Bedford Channel across McMillan Island. The national historic site contains a visitor centre and a largely reconstructed trading post that contains ten structures surrounded by wooden palisades.

British Columbia

British Columbia

British Columbia, commonly abbreviated as BC, is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east, the territories of Yukon and Northwest Territories to the north, and the US states of Washington, Idaho and Montana to the south and Alaska to the northwest. With an estimated population of 5.3 million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6 million people in Metro Vancouver.

Hudson's Bay Company

Hudson's Bay Company

The Hudson's Bay Company is a Canadian retail business group. A fur trading business for much of its existence, it became the largest and oldest corporation in Canada, and now owns and operates retail stores across the country. The company's namesake business division is Hudson's Bay, commonly referred to as The Bay.

Uses

The Fraser is heavily exploited by human activities, especially in its lower reaches. Its banks are rich farmland, its water is used by pulp mills, and a few dams on some tributaries provide hydroelectric power. The main flow of the Fraser has never been dammed partly because its high level of sediment flows would result in a short dam lifespan, but mostly because of strong opposition from fisheries and other environmental concerns. In 1858, the Fraser River and surrounding areas were occupied when the gold rush came to the Fraser Canyon and the Fraser River. It is also a popular fishing location for residents of the Lower Mainland.

The delta of the river, especially in the Boundary Bay area, is an important stopover location for migrating shorebirds.[23]

The Fraser Herald, a regional position within the Canadian Heraldic Authority is named after the river.

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Pulp mill

Pulp mill

A pulp mill is a manufacturing facility that converts wood chips or other plant fiber sources into a thick fiber board which can be shipped to a paper mill for further processing. Pulp can be manufactured using mechanical, semi-chemical, or fully chemical methods. The finished product may be either bleached or non-bleached, depending on the customer requirements.

Boundary Bay

Boundary Bay

Boundary Bay is a shallow bay situated on the Pacific coast of North America on the Canada–United States border between the Canadian province of British Columbia and the U.S. state of Washington.

Bird migration

Bird migration

Bird migration is the regular seasonal movement, often north and south, along a flyway, between breeding and wintering grounds. Many species of bird migrate. Migration carries high costs in predation and mortality, including from hunting by humans, and is driven primarily by the availability of food. It occurs mainly in the northern hemisphere, where birds are funneled onto specific routes by natural barriers such as the Mediterranean Sea or the Caribbean Sea.

Fraser Herald

Fraser Herald

Fraser Herald of Arms is the title of one of the officers of arms at the Canadian Heraldic Authority in Ottawa. Like the other heralds at the Authority, the name is derived from the Canadian river of the same name. Since the inception of the office, Fraser Herald of Arms has been the principal artist of the Canadian Heraldic Authority. As such, Fraser is responsible for overseeing the artwork created for all grants of arms emanating from the Authority.

Canadian Heraldic Authority

Canadian Heraldic Authority

The Canadian Heraldic Authority is part of the Canadian honours system under the Canadian monarch, whose authority is exercised by the Governor General of Canada. The authority is responsible for the creation and granting of new coats of arms, flags, and badges for Canadian citizens, government agencies, municipal, civic and other corporate bodies. The authority also registers existing armorial bearings granted by other recognized heraldic authorities, approves military badges, flags, and other insignia of the Canadian Forces, and provides information on heraldic practices. It is well known for its innovative designs, many incorporating First Nations symbolism.

Fishing

The Fraser River is known for the fishing of white sturgeon, all five species of Pacific salmon (chinook, coho, chum, pink, sockeye), as well as steelhead trout. The Fraser River is also the largest producer of salmon in Canada.[24] A typical white sturgeon catch can average about 500 pounds (230 kg).[25] A white sturgeon weighing an estimated 500 kilograms (1,100 lb) and measuring 3.76 metres (12 ft 4 in) was caught and released on the Fraser River in July 2012.[26] In 2021, a white sturgeon was caught on the river weighing 890 pounds (400 kg), with a length of 352 cm (11.55 ft). It was estimated to be over 100 years old. The fish was tagged and released.[27]

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White sturgeon

White sturgeon

White sturgeon is a species of sturgeon in the family Acipenseridae of the order Acipenseriformes. They are an anadromous fish species ranging in the Eastern Pacific; from the Gulf of Alaska to Monterey, California. However, some are landlocked in the Columbia River Drainage, Montana, and Lake Shasta in California, with reported sightings in northern Baja California, Mexico.

Chinook salmon

Chinook salmon

The Chinook salmon is the largest and most valuable species of Pacific salmon in North America, as well as the largest in the genus Oncorhynchus. Its common name is derived from the Chinookan peoples. Other vernacular names for the species include king salmon, Quinnat salmon, Tsumen, spring salmon, chrome hog, Blackmouth, and Tyee salmon. The scientific species name is based on the Russian common name chavycha (чавыча).

Chum salmon

Chum salmon

The chum salmon, also known as dog salmon or keta salmon, is a species of anadromous salmonid fish from the genus Oncorhynchus native to the coastal rivers of the North Pacific and the Beringian Arctic, and is often marketed under the trade name silverbrite salmon in North America. The English name "chum salmon" comes from the Chinook Jargon term tzum, meaning "spotted" or "marked"; while keta in the scientific name comes from Russian, which in turn comes from the Evenki language of Eastern Siberia.

Pink salmon

Pink salmon

Pink salmon or humpback salmon is a species of anadromous fish in the salmon family. It is the smallest and most abundant of the Pacific salmon. The scientific species name is based on the Russian common name for this species gorbúša (горбуша), which literally means humpie.

Flooding

The most significant Fraser river floods in recorded history occurred in 1894 and 1948. [28][29]

1894 flood

The Chilliwack flood of 1894
The Chilliwack flood of 1894

After European settlement, the first disastrous flood in the Lower Mainland (Fraser Valley and Metro Vancouver) occurred in 1894.[30][31] With no protection against the rising waters of the Fraser River, Fraser Valley and Metro Vancouver communities from Chilliwack downstream were inundated with water. In the 1894 floods, the water mark at Mission reached 7.85 metres (25.75 ft).

After the 1894 flood, a dyking system was constructed throughout the Fraser Valley. The dyking and drainage projects greatly improved the flood problems, but unfortunately over time, the dykes were allowed to fall into disrepair and became overgrown with brush and trees. With some dykes constructed of a wooden frame, they gave way in 1948 in several locations, marking the second disastrous flood. Flooding since 1948 has been minor in comparison.

1948 flood

1948 saw massive flooding in Chilliwack and other areas along the Fraser River.[32] The high-water mark at Mission rose to 7.5 metres (24.7 ft). The peak flow was about 15,600 cubic meters per second.

Timeline

  • On May 28, 1948, the Semiault Creek Dyke broke.
  • On May 29, 1948, dykes near Glendale (now Cottonwood Corners) gave way and in four days, 49 square kilometres (12,000 acres) of fertile ground were under water.
  • On June 1, 1948, the Cannor Dyke (east of Vedder Canal near Trans Canada Highway) broke and released tons of Fraser River water onto the Greendale area, destroying homes and fields.
  • On June 3, 1948, the steamer Gladys supplied flood-stricken Chilliwack with tents and provisions as well as moving people and stock onto high ground.

Causes

Cool temperatures in March, April, and early May had delayed the melting of the heavy snowpack that had accumulated over the winter season. Several days of hot weather and warm rains over the holiday weekend in late May hastened the thawing of the snowpack. Rivers and streams quickly swelled with spring runoff, reaching heights surpassed only in 1894. Finally, the poorly maintained dyke systems failed to contain the water.

At the height of the 1948 flood, 200 square kilometres (50,000 acres) stood under water. Dykes broke at Agassiz, Chiliwack, Nicomen Island, Glen Valley and Matsqui. When the flood waters receded a month later, 16,000 people had been evacuated, with damages totaling $20 million, about $225 million in 2020 dollars.

1972 flood

Major flooding occurred once again in 1972 due to a significant spring freshet, primarily impacting regions around Prince George, Kamloops, Hope and Surrey.[33][34][35][36]

2007 flood

Due to record snowpacks on the mountains in the Fraser River catch basin which began melting, combined with heavy rainfall, water levels on the Fraser River rose in 2007 to a level not reached since 1972.[37] Low-lying land in areas upriver such as Prince George suffered minor flooding. Evacuation alerts were given for the low-lying areas not protected by dikes in the Lower Mainland.[38] However, the water levels did not breach the dikes, and major flooding was averted.

2021 flood

Major flooding occurred in November 2021 as part of the November 2021 Pacific Northwest floods.

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Lower Mainland

Lower Mainland

The Lower Mainland is a geographic and cultural region of the mainland coast of British Columbia that generally comprises the regional districts of Metro Vancouver and Fraser Valley. Home to approximately 3.05 million people as of the 2021 Canadian census, the Lower Mainland contains sixteen of the province's 30 most populous municipalities and approximately 60% of the province's total population.

Fraser Valley Regional District

Fraser Valley Regional District

The Fraser Valley Regional District (FVRD) is a regional district in British Columbia, Canada. Its headquarters are in the city of Chilliwack. The FVRD covers an area of 13,361.74 km² (5,159 sq mi). It was created in 1995 by an amalgamation of the Fraser-Cheam Regional District and Central Fraser Valley Regional District and the portion of the Dewdney-Alouette Regional District from and including the District of Mission eastwards.

Metro Vancouver Regional District

Metro Vancouver Regional District

The Metro Vancouver Regional District (MVRD), or simply Metro Vancouver, is a Canadian political subdivision and corporate entity representing the metropolitan area of Greater Vancouver, designated by provincial legislation as one of the 28 regional districts in British Columbia. The organization was known as the Regional District of Fraser–Burrard for nearly one year upon incorporating in 1967, and as the Greater Vancouver Regional District (GVRD) from 1968 to 2017.

Levee

Levee

A levee, dike, dyke, embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines.

Fraser River flood of 1948

Fraser River flood of 1948

The Fraser River flood of 1948 was the most devastating flooding to hit Greater Vancouver in living memory. In that years floods, more than 2,300 homes were destroyed, and 16,00 people displaced, as well as a great number of livestock killed. The population of the Lower Fraser Valley at the time was only around 50,000. At the floods height, the water level measured 7.6m. The areas of Abbotsford and northern Langley were particularly hard-hit. The Canadian National Railway line and the Trans-Canada Highway rail lines were flooded, cutting southwestern B.C. off from the rest of Canada. When the waters receded, 10 were dead, 1,500 were left homeless, and between $150-$210 million in damage had been inflicted on the area

Freshet

Freshet

The term freshet is most commonly used to describe a snowmelt, an annual high water event on rivers resulting from snow and river ice melting. A spring freshet can sometimes last several weeks on large river systems, resulting in significant inundation of flood plains as the snowpack melts in the river's watershed. Freshets can occur with differing strength and duration depending upon the depth of the snowpack and the local average rates of warming temperatures. Deeper snowpacks which melt quickly can result in more severe flooding. Late spring melts allow for faster flooding; this is because the relatively longer days and higher solar angle allow for average melting temperatures to be reached quickly, causing snow to melt rapidly. Snowpacks at higher altitudes and in mountainous areas remain cold and tend to melt over a longer period of time and thus do not contribute to major flooding. Serious flooding from southern freshets are more often related to rain storms of large tropical weather systems rolling in from the South Atlantic or Gulf of Mexico, to add their powerful heating capacity to lesser snow packs. Tropically induced rainfall influenced quick melts can also affect snow cover to latitudes as far north as southern Canada, so long as the generally colder air mass is not blocking northward movement of low pressure systems.

Prince George, British Columbia

Prince George, British Columbia

Prince George is a city in British Columbia, Canada, with a city population of 76,708 and a metro census agglomeration population of 89,490. It is often called the province's "northern capital". It is situated at the confluence of the Fraser and Nechako rivers.

Kamloops

Kamloops

Kamloops is a city in south-central British Columbia, Canada, at the confluence of the South flowing North Thompson River and the West flowing Thompson River, east of Kamloops Lake. It is located in the Thompson-Nicola Regional District, whose district offices are based here. The surrounding region is sometimes referred to as the Thompson Country.

Hope, British Columbia

Hope, British Columbia

Hope is a district municipality at the confluence of the Fraser and Coquihalla rivers in the province of British Columbia, Canada. Hope is at the eastern end of both the Fraser Valley and the Lower Mainland region, and is at the southern end of the Fraser Canyon. To the east, over the Cascade Mountains, is the Interior region, beginning with the Similkameen Country on the farther side of the Allison Pass in Manning Park. Located 154 kilometres (96 mi) east of Vancouver, Hope is at the southern terminus of the Coquihalla Highway and the western terminus of the Crowsnest Highway, locally known as the Hope-Princeton, where they merge with the Trans-Canada Highway. Hope is at the eastern terminus of Highway 7. As it lies at the eastern end of the Fraser Valley in the windward Cascade foothills, the town gets very high amounts of rain and cloud cover – particularly throughout the autumn and winter.

Surrey, British Columbia

Surrey, British Columbia

Surrey is a city in British Columbia, Canada. It is located south of the Fraser River on the Canada–United States border. It is a member municipality of the Metro Vancouver regional district and metropolitan area. Mainly a suburban city, Surrey is the province's second-largest by population after Vancouver and the third-largest by area after Abbotsford and Prince George. Seven neighbourhoods in Surrey are designated town centres: Cloverdale, Fleetwood, Guildford, Newton, South Surrey, and City Centre encompassed by Whalley.

November 2021 Pacific Northwest floods

November 2021 Pacific Northwest floods

The 2021 Pacific Northwest floods comprise a series of floods that affected British Columbia, Canada, and parts of neighboring Washington state in the United States. The flooding and numerous mass wasting events were caused by a Pineapple Express, a type of atmospheric river, which brought heavy rain to parts of southern British Columbia and northwestern United States. The natural disaster prompted a state of emergency for the province of British Columbia.

Tributaries

Fraser River in the Glen Fraser area, about 25 kilometres (16 mi) upstream of Lillooet
Fraser River in the Glen Fraser area, about 25 kilometres (16 mi) upstream of Lillooet
An east-facing aerial view of Ladner beyond Barber Island, Duck Island, Gunn Island and Port Guichon in the Fraser River Estuary
An east-facing aerial view of Ladner beyond Barber Island, Duck Island, Gunn Island and Port Guichon in the Fraser River Estuary

Tributaries are listed from the mouth of the Fraser and going up river.

Fraser River as seen from the grounds of Westminster Abbey, above Hatzic in Mission, British Columbia. Sumas Mountain in background.
Fraser River as seen from the grounds of Westminster Abbey, above Hatzic in Mission, British Columbia. Sumas Mountain in background.

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Ladner, British Columbia

Ladner, British Columbia

Ladner is a part of the City of Delta, British Columbia, Canada, and a suburb of Vancouver, British Columbia. It was created as a fishing village on the banks of the Fraser River.

List of tributaries of the Fraser River

List of tributaries of the Fraser River

This is a partial listing of tributaries of the Fraser River. Tributaries and sub-tributaries are hierarchically listed in upstream order from the mouth of the Fraser River. The list may also include streams known as creeks and sloughs. Lakes are noted in italics.

Brunette River

Brunette River

The Brunette River runs through East Burnaby, New Westminster and Coquitlam, flowing out of Burnaby Lake and to the Fraser River. It is the final outflow of the Central Valley Watershed, which consists of most streams between the Ulksen and Burnaby Heights. According to a map and materials by Heritage Advisory Committee and Environment and Waste Management Committee of the City of Burnaby (1993), the number of native campsites discovered on the shores of the Fraser River, Burrard Inlet and Deer Lake and some petroglyphs suggest that the area was used extensively by local aboriginal peoples such as the Squamish, Musqueam and Kwantlen for hunting and fishing before the arrival of European settlers.

Coquitlam River

Coquitlam River

The Coquitlam River is a tributary of the Fraser River in the Canadian province of British Columbia. The river's name comes from the word Kʷikʷəƛ̓əm which translates to "Red fish up the river". The name is a reference to a sockeye salmon species that once occupied the river's waters.

Pitt River

Pitt River

The Pitt River in British Columbia, Canada is a large tributary of the Fraser River, entering it a few miles upstream from New Westminster and about 25 km ESE of Downtown Vancouver. The river, which begins in the Garibaldi Ranges of the Coast Mountains, is in two sections above and below Pitt Lake and flows on a generally southernly course. Pitt Lake and the lower Pitt River are tidal in nature as the Fraser's mouth is only a few miles downstream from their confluence.

Kanaka Creek

Kanaka Creek

Kanaka Creek is a tributary of the Fraser River, in the Canadian province of British Columbia. It flows through Maple Ridge, a district municipality at the eastern edge of Metro Vancouver.

D'Herbomez Creek

D'Herbomez Creek

D'Herbomez Creek is a creek in eastern Mission, British Columbia, flowing southeast to join the Fraser River at the Pekw'Xe:yles Indian Reserve.

Norrish Creek

Norrish Creek

Norrish Creek is a tributary of the Fraser River. It is located in the Douglas Ranges, the southernmost subrange of the Pacific Ranges of the Coast Mountains of British Columbia, Canada to the north of Nicomen Island. Local residents refer to it as "Suicide Creek." It was named after William Henry Norrish a pioneer Scottish Canadian farmer.

Harrison River

Harrison River

The Harrison River is a short but large tributary of the Fraser River, entering it near the community of Chehalis, British Columbia, Canada. The Harrison drains Harrison Lake and is the de facto continuation of the Lillooet River, which feeds the lake.

Coquihalla River

Coquihalla River

The Coquihalla River is a tributary of the Fraser River in the Cascade Mountains of the Canadian province of British Columbia. It originates in the Coquihalla Lakes and empties into the Fraser River at Hope.

Anderson River (British Columbia)

Anderson River (British Columbia)

The Anderson River is a tributary of the Fraser River in the Canadian province of British Columbia.

Nahatlatch River

Nahatlatch River

The Nahatlatch River is a tributary of the Fraser River in the Canadian province of British Columbia. It originates in the Lillooet Ranges of the Coast Mountains and empties into the Fraser River in the Fraser Canyon, north of Boston Bar.

Source: "Fraser River", Wikipedia, Wikimedia Foundation, (2023, March 20th), https://en.wikipedia.org/wiki/Fraser_River.

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References
  1. ^ Salishan languages and Chinook Jargon. The Halkomelem form is Sto:lo, used as the name of the people of the Fraser Valley stretch of the river. "Staulo" is the anglicization used in the Kamloops Wawa lexicon of the Chinook Jargon
  2. ^ Carrier language. Lhtako is also used to mean the Dakelh people of the Quesnel/North Cariboo area
  3. ^ Indigenous name recorded by Alexander Mackenzie on expedition to find Columbia River’s headwaters; circa 18-?
  4. ^ Tsilhqot'in name meaning Sturgeon (ʔElhdachogh) River (Yeqox)
  5. ^ a b c "Fraser River Fact Sheet". Canadian Heritage Rivers System. Archived from the original on July 12, 2017. Retrieved December 2, 2016.
  6. ^ Ambient Water Quality Assessment and Objectives for the Fraser River sub-basin from Kanaka Creek to the Mouth Archived March 4, 2016, at the Wayback Machine, BC Ministry of Environment
  7. ^ a b c "Comprehensive Review of Fraser River at Hope: Flood Hydrology and Flows, Scoping Study Final Report" (PDF). BC Ministry of Environment. October 2008. Retrieved October 11, 2009.
  8. ^ "Fraser River Delta". Ramsar Sites Information Service. Retrieved April 25, 2018.
  9. ^ "BC Geographical Names". Retrieved June 2, 2019.
  10. ^ Cannings, Richard and Sidney. British Columbia: A Natural History. p.41. Greystone Books. Vancouver. 1996
  11. ^ "Dakleh Placenames". www.ydli.org.
  12. ^ "North Arm Fraser River". BC Geographical Names.
  13. ^ Mass, Cliff (2008). The Weather of the Pacific Northwest. University of Washington Press. pp. 146–148. ISBN 978-0-295-98847-4.
  14. ^ "Description". Western Hemisphere Shorebird Reserve Network. Retrieved February 18, 2008.
  15. ^ Real-Time Hydrometric Data Map Search – Water Level and Flow – Environment Canada
  16. ^ "Ambient Water Quality Assessment and Objectives for the Fraser River Sub-basin from Kanaka Creek to the Mouth". British Columbia Ministry of Environment, Water Management Branch, Resource Quality Section. November 1985. Archived from the original on March 4, 2016. Retrieved October 11, 2009.
  17. ^ a b Ferguson, John W.; Michael Healey (May 2009). "Hydropower in the Fraser and Columbia Rivers". Catch and Culture (newsletter). Mekong River Commission. Archived from the original on February 15, 2010. Retrieved October 11, 2009.
  18. ^ Hayes, Derek (1999). Historical Atlas of the Pacific Northwest: Maps of exploration and Discovery. Sasquatch Books. ISBN 1-57061-215-3.
  19. ^ Maclachlan, Morag (November 1, 2011). "Journal Kept by George Barnston, 1827-8". Fort Langley Journals, 1827-30. UBC Press. p. 23. ISBN 978-0774841979.
  20. ^ "Modest beginnings." "The Orca," February 2020
  21. ^ Mackie, Richard Somerset (1997). Trading Beyond the Mountains: The British Fur Trade on the Pacific 1793–1843. Vancouver: University of British Columbia (UBC) Press. p. 58. ISBN 0-7748-0613-3.
  22. ^ "Fraser River". Canadian Council for Geographic Education. Archived from the original on April 17, 2005.
  23. ^ "Welcome". www.reifelbirdsanctuary.com.
  24. ^ Lapointe, Mike; Cooke, Steven J.; Hinch, Scott G.; Farrell, Anthony P.; Jones, Simon; MacDonald, Steve; Patterson, David; Healey, Michael C.; Van Der Kraak, Glen (2003). "Late-run sockeye salmon in the Fraser River, British Columbia are experiencing early upstream migration and unusually high rates of mortality: what is going on" (PDF). Proceedings of the 2003 Georgia Basin/Puget Sound Research Conference, Vancouver, BC. 31: 1–14.
  25. ^ "Sturgeon Weight/Age Chart". Rivermen Rod and Gun Club.
  26. ^ "Giant 12 foot Sturgeon caught on Fraser River « Great River Fishing Adventures". greatriverfishing.com.
  27. ^ "Record sturgeon catch on Fraser River 'a lifetime moment' for ex-NHL goalie and friends". vancouversun.
  28. ^ "PHOTOS: Looking back at the floods of 1894 and 1948 in Chilliwack". The Chilliwack Progress. June 14, 2020. Retrieved November 29, 2021.
  29. ^ "River flooding part of Hope history". Hope Standard. June 27, 2012. Retrieved November 29, 2021.
  30. ^ "Flooding events in Canada: British Columbia". Government of Canada. December 2, 2010. Retrieved November 29, 2021. The greatest Fraser River flood in the past century occurred in 1894, when the floodplain areas were in the very early stages of settlement and development.
  31. ^ "North Delta history: The historic floods of May". Surrey Now Leader. May 12, 2019. Retrieved November 29, 2021. In May of 1894, the Fraser River had its largest recorded flood; Abbotsford and Chilliwack were particularly hard hit. North Delta lay above the flood waters, but farmers in South Westminster to the north and Ladner to the south faced weeks of their land and homes inundated with murky silt-laden water.
  32. ^ "Flooding events in Canada: British Columbia". Government of Canada. December 2, 2010. Retrieved November 29, 2021. On June 10, 1948, the Fraser reached a peak elevation of 7.6 metres at Mission. Before the waters receded, over a dozen dyking systems had been breached and more than 22 000 hectares, nearly one third of the entire lower Fraser Valley floodplain area, had been flooded to this depth. The floodwaters severed the two transcontinental rail lines; inundated the Trans-Canada Highway; flooded urban areas such as Agassiz, Rosedale, and parts of Mission, forcing many industries to close or reduce production; and deposited a layer of silt, driftwood and other debris over the entire area.
  33. ^ "Flooding events in Canada: British Columbia". Government of Canada. December 2, 2010. Retrieved November 29, 2021. On June 16, the lower Fraser peaked at Hope, with a maximum instantaneous flow of 3400 cubic metres per second and a maximum elevation of 7.1 metres, well above the danger level of 6.1 metres. Damage on the Fraser in 1972 amounted to $10 million ($36.9 million in 1998 dollars) and occurred mainly in the upstream communities of Prince George and Kamloops, and in the Surrey area of the lower Fraser Valley.
  34. ^ "River flooding part of Hope history". Hope Standard. June 27, 2012. Retrieved November 29, 2021. In 1972, the Fraser River again experienced record flood waters – the second highest in recorded times with a discharge of 12,900 cubic metres per second and a maximum height of 10.141 meters at Hope on June 16. Wardle Street and part of Seventh Avenue were submerged, and on Tom Berry Road 10 houses were flooded and families were forced to evacuate their properties. Pumps were brought in to remove water and residents were able to return home after approximately a week.
  35. ^ "North Delta history: The historic floods of May". Surrey Now Leader. May 12, 2019. Retrieved November 29, 2021. When waters again rose in 1972, flood conditions were more reasonable controlled, with dykes, prediction and timely sandbagging. However, there was still $10 million of damage, mainly in Prince George and Surrey.
  36. ^ "Fraser River Floodplain". City of Surrey. December 11, 2019. Retrieved November 29, 2021. The area flooded again in 1972 and this is why in 1975 the South Westminster Dyking District transferred to Surrey under an agreement with the province to improve the existing dyke and flood protection systems.
  37. ^ River Water Still Rising Archived October 6, 2007, at the Wayback Machine. Prince George Free Press, June 6, 2006.
  38. ^ Fraser flood alert imminent Mission gauge under close scrutiny, river likely to peak at 7.5 m by Saturday Archived September 28, 2007, at the Wayback Machine. Langley Times, June 6, 2007.
Further reading
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