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97-861: Discovery II began its life in 1953 as the Yutana , a freight boat hauling goods on the Yukon and Tanana rivers (hence its name, a combination of the names of the two rivers). Captain Jim Binkley purchased the Yutana in 1967 after its effective freighting life was over, and until 1970 it was drydocked on the Chena River near Fairbanks, Alaska. In 1971, Jim Binkley was in need of a larger sternwheel riverboat with which to conduct his daily river tours (his first sternwheeler, Discovery I , frequently reached its maximum capacity of 150 passengers), and decided to convert

194-664: A Holikachuk phrase that means big river . Then, two years later, the Gwich'ins told the Hudson's Bay Company that their name for the river was Yukon and that the name meant white water river . White water river in fact corresponds to Gwich'in words that can be shortened to form Yukon . Because the Holikachuks had been trading regularly with both the Gwich’ins and the Yup'iks ,

291-454: A cooperative effort of 70 First Nations and tribes in Alaska and Canada, has the goal of making the river and its tributaries safe to drink from again by supplementing and scrutinizing government data. The name Yukon , or ųųg han , is a contraction of the words in the Gwich'in phrase chųų gąįį han , which means white water river and refers to "the pale colour" of glacial runoff in

388-639: A passenger capacity of 900, went into service in July 1987. After Discovery III took over as the Riverboat Discovery's primary tour vessel, the Discovery II went into drydock for repairs and renovation. After approximately 10 years on the drydock, Discovery II was relicensed and brought back into service in 1999 in preparation for the Riverboat Discovery's fiftieth anniversary, as well as to handle an increased number of passengers serviced by

485-414: A single mechanical delay. By the mid-1980s, however, a growing tourism industry meant that Discovery II , like Discovery I before it, was becoming too small for the Riverboat Discovery's needs. The increased number of passengers straining Discovery II 's capacity precipitated the design and construction of the third Riverboat Discovery sternwheeler, Discovery III , in 1986-1987. Discovery III , with

582-528: A steady decline since the 1960s. Water mammals such as beavers and muskrats are extremely common in the Mackenzie Delta and surrounding areas of muskeg. The Mackenzie estuary is also a calving area for beluga whales . The Mackenzie valley is believed to have been the path taken by prehistoric peoples during the initial human migration from Asia to North America more than 10,000 years ago. However, archaeological evidence of human habitation along

679-543: Is 1,738 kilometres (1,080 mi) long, flowing north-northwest from Great Slave Lake into the Arctic Ocean , where it forms a large delta at its mouth. Its extensive watershed drains about 20 percent of Canada. It is the largest river flowing into the Arctic from North America , and including its tributaries has a total length of 4,241 kilometres (2,635 mi), making it the thirteenth longest river system in

776-838: Is a river in the Canadian boreal forest . It forms, along with the Slave, Peace, and Finlay, the longest river system in Canada , and includes the second largest drainage basin of any North American river after the Mississippi . The Mackenzie River flows through a vast, thinly populated region of forest and tundra entirely within the Northwest Territories in Canada, although its many tributaries reach into five other Canadian provinces and territories . The river's main stem

873-512: Is accessible from the Yukon at Pitkas Point), and Mountain Village . After Mountain Village, the main Yukon channel frays into many channels, sprawling across the delta. There are a number of communities after the "head of passes," as the channel division is called locally: Nunum Iqua , Alakanuk , Emmonak , and Kotlik . Of those delta communities, Emmonak is the largest with roughly 760 people in

970-533: Is also performed along the river in summer by barge , enabling heavy goods, oil, and vehicles to be transported to communities along the Yukon, Tanana, Innoko, and Koyukuk rivers. This service is performed by Ruby Marine and reaches Tanana on the Yukon River and Nenana on the Tanana River. Some of the upper slopes of this watershed (e.g. Nulato Hills ) are forested by Black Spruce . This locale near

1067-649: Is considered to be some of the best northern farmland in Canada, due to the high concentration of minerals found in the soil. These conditions are expected to be improved even more by trends in climate change, such as warmer temperatures and a longer growing season. According to the British Columbia Environmental Network, "there is enough agricultural capability in the Peace River Valley to provide vegetables to all of northern Canada". The only functioning oil pipeline in

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1164-526: Is forested (mostly boreal forest ). Wetlands comprise about 18%, or about 324,900 km (125,400 sq mi), of the basin. More than 93% of forested areas are virgin old-growth forest . However, human activities such as oil extraction have threatened water quality in the headwaters of the Mackenzie River. In addition, a warming climate in northern parts of the watershed is melting permafrost and destabilizing soil through erosion. Most of

1261-426: Is formed by the confluence of the two rivers and flows 415 kilometres (258 mi) due north into Great Slave Lake, at Fort Resolution , Northwest Territories. The Slave is by far the largest river flowing into the lake, with an annual flow of 108 km (87 million acre-feet). It contributes about 77% of the overall inflow, and forms a large delta where it enters the lake. Other rivers entering Great Slave Lake are

1358-539: Is known as Mills Lake. After heading west for about 100 km (62 mi) the Mackenzie narrows and turns northwest through a long stretch of fast water and rapids, past the village of Jean Marie River . At Fort Simpson it is joined by the Liard River , its biggest direct tributary, from the west. The Liard drains a large area in the southern Yukon and northern BC and carries a large amount of sediment during

1455-541: Is more than 25% larger than Texas or Alberta . The longest river in Alaska and Yukon, it was one of the principal means of transportation during the 1896–1903 Klondike Gold Rush . A portion of the river in Yukon—"The Thirty Mile" section, from Lake Laberge to the Teslin River —is a national heritage river and a unit of Klondike Gold Rush International Historical Park . Paddle-wheel riverboats continued to ply

1552-562: Is nearly 210 km (130 mi) from north to south, and ranges in width from 50 to 80 km (31 to 50 mi). It is the second biggest Arctic delta in the world, after the Lena River delta in Russia. Most land in the Mackenzie delta consists of permafrost , with great depths to bedrock. A characteristic feature of the delta is its numerous pingos , or hills of earth-covered-ice – some 1,400 of them. The Peel River , carrying much of

1649-678: Is significantly deeper than Great Bear. The third major lake, Athabasca, is less than a third that size with an area of 7,800 km (3,000 sq mi). Six other lakes in the watershed cover more than 1,000 km (390 sq mi), including the Williston Lake reservoir , the second-largest artificial lake in North America, on the Peace River. The river discharges more than 325 cubic kilometres (78 cu mi) of water each year, accounting for roughly 11% of

1746-592: Is very young in geologic terms – its channel formed over a period of no more than several thousand years as the ice sheet retreated. Prior to the ice ages, only the Peel River tributary flowed through what is now the Mackenzie Delta into the Arctic Ocean. The other tributaries of the Mackenzie combined into the "Bell River" which flowed east into Hudson Bay. During glaciation the weight of the ice sheet depressed northern Canada's terrain to such an extent that when

1843-618: The 1825–1827 Mackenzie River expedition . The following year he traced the coast west until blocked by ice while John Richardson followed the coast east to the Coppermine River . In 1849 William Pullen reached the Mackenzie from the Bering Strait. In the following decades the North West Company established forts on the river, the precursors of present-day settlements such as Fort Simpson (formerly Fort of

1940-538: The Arctic Red River from the southwest at Tsiigehtchic , where traffic on the Dempster Highway crosses via ferry/ice bridge. About 30 kilometres (19 mi) northwest of Tsiigehtchic is Point Separation, the head of the vast Mackenzie River Delta, whose branching channels, ponds and wetlands spread across more than 12,000 square kilometres (4,600 sq mi) of the coastal plain. The delta

2037-888: The Athabasca River all the way to the delta, though with several areas such as the huge rapids on the Slave River requiring portages . The route taken by gold seekers started in Edmonton and followed the Athabasca, Slave and Mackenzie Rivers as far as the Peel River , then up the Peel and its tributary the Rat River to the headwaters of the Porcupine River , which flows to the Yukon River . Many who attempted

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2134-762: The Bering Strait ; and the Fraser River and Columbia River systems, both of which empty into the Pacific Ocean . Lowland divides in the north separate the Mackenzie basin from the Arctic Ocean watersheds of the Anderson , Horton , Coppermine and Back Rivers. In the east, the Mackenzie borders on the Hudson Bay watersheds of the Thelon and Churchill Rivers, and to the south it is bordered by

2231-634: The Chilkoot Trail . Either way, Atlin Lake flows into Tagish Lake (via the Atlin River), as eventually does Lake Lindeman after flowing into Bennett Lake . Tagish Lake then flows into Marsh Lake (via the Tagish River). The Yukon River proper starts at the northern end of Marsh Lake, just south of Whitehorse . Some argue that the source of the Yukon River should really be Teslin Lake and

2328-492: The Environmental Protection Agency does not list the Yukon River among its impaired watersheds, and water-quality data from the U.S. Geological Survey shows relatively good levels of turbidity, metals, and dissolved oxygen. The Yukon and Mackenzie rivers have much higher suspended sediment concentrations than the great Siberian Arctic rivers. The Yukon River Inter-Tribal Watershed Council ,

2425-588: The Gwichya Gwich'in . In 2008, Canadian and Japanese researchers extracted a constant stream of natural gas from a test project at the Mallik methane hydrate field in the Mackenzie Delta. This was the second such drilling at Mallik: the first took place in 2002 and used heat to release methane. In the 2008 experiment, researchers were able to extract gas by lowering the pressure, without heating, requiring significantly less energy. The Mallik gas hydrate field

2522-649: The Northern Interior of BC, is the ultimate source of the Mackenzie River via the Finlay – Peace River system, which stretches 1,923 kilometres (1,195 mi) through BC and Alberta. The 1,231-kilometre (765 mi) Athabasca River originates further south, in Jasper National Park in southwest Alberta. Together, the Peace and Athabasca rivers drain a significant portion of the eastern slope of

2619-568: The Rocky Mountains and the central Alberta prairie. The Peace contributes the majority of the water, about 66 km (54 million acre-feet ) per year, and the Athabasca contributes 25 km (20 million acre-feet). The Peace and Athabasca meet at the Peace-Athabasca Delta , a vast inland delta at the western end of Lake Athabasca , which also takes runoff from the northern third of Saskatchewan. The Slave River

2716-758: The Saskatchewan – Nelson River system, which also empties into Hudson Bay. The Mackenzie system is hydrologically connected to the Hudson Bay watershed via Wollaston Lake , which is not only the source of the Fond du Lac tributary of Lake Athabasca, but also of the Cochrane River , which flows east into the Churchill River. The eastern portion of the Mackenzie basin is dominated by vast reaches of lake-studded boreal forest and includes many of

2813-549: The Seward Peninsula represents the near westernmost limit of the Black Spruce, Picea mariana , one of the most widespread conifers in northern North America. The river flows into several parklands and refuges including: Yukon at Pilot Station (121 miles upstream of mouth) minimum, average and maximum discharge: for statistical calculation The Yukon River is home to one of the longest salmon runs in

2910-623: The Takhini River ) and Kluane Lake (into the Kluane and then White River). The river passes through the communities of Whitehorse , Carmacks , (just before the Five Finger Rapids ) and Dawson City in Yukon , and crossing Alaska into Eagle , Circle , Fort Yukon , Stevens Village , Rampart , Tanana , Ruby , Galena , Nulato , Grayling , Holy Cross , Russian Mission , Marshall , Pilot Station , St. Marys (which

3007-455: The Taltson , Lockhart and Hay Rivers , the latter of which also extends into Alberta and BC. The Mackenzie River issues from the western end of Great Slave Lake about 150 km (93 mi) south-west of Yellowknife . The channel is initially several kilometres wide but narrows to about 800 m (2,600 ft) at Fort Providence , which was historically an important ferry crossing in

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3104-493: The Teslin River , which has a larger flow when it reaches the Yukon at Hootalinqua. The upper end of the Yukon River was originally known as the Lewes River until it was established that it actually was the Yukon. North of Whitehorse, the Yukon River widens into Lake Laberge , made famous by Robert W. Service 's " The Cremation of Sam McGee ". Other large lakes that are part of the Yukon River system include Kusawa Lake (into

3201-538: The Yutana into a passenger vessel. Together with his friend Iver Johnson, Jim Binkley renovated the Yutana and rechristened her the Discovery II . She went into service immediately upon the completion of the conversion. For the following fifteen years, Discovery II was the Riverboat Discovery's primary tour vessel; her passenger capacity was nearly 400, a more than twofold increase over Discovery I . In addition to increased capacity, Discovery II also proved mechanically reliable, embarking on over 5,000 trips without

3298-416: The 2000 census. Emmonak's gravel airstrip is the regional hub for flights. Navigational obstacles on the Yukon River are the Five Finger Rapids and Rink Rapids downstream from Carmacks. Despite its length, there are only four vehicle-carrying bridges across the river, listed from upstream to downstream: A car ferry crosses the river at Dawson City in the summer; it is replaced by an ice bridge over

3395-453: The 3,200-kilometre (2,000 mi) journey died along the way or turned back before reaching the Yukon. Oil was discovered at Norman Wells in the 1920s, beginning a period of industrialization in the Mackenzie valley. Oil was initially shipped out by steamboats, supplying mines and towns across the NWT. This demand grew when gold was discovered on the northern shore of Great Slave Lake, leading to

3492-516: The Alaska Department of Fish & Game's Division of Commercial Fisheries banned all fishing of Chinook and chum salmon, including for subsistence. Various organizations are involved to protect healthy salmon runs into the future. The Yukon River Drainage Fisheries Association was formed in 1990 by a consensus of fishers representing the entire drainage in response to recent disaster years. Its organizational goals include giving voice to

3589-451: The Forks). A lucrative fur trade was carried out, as the Mackenzie basin teemed with beaver and muskrat. However, the short summer and harsh winter conditions limited trappers' activities. During the late 19th century Fort Simpson was regional headquarters for the Hudson's Bay Company . The first fur trappers were native, but starting in the 1920s increasing numbers of European trappers entered

3686-579: The Great Slave Lake region. By acting as a massive stabilizer on the water flow of the Peace River, Williston Lake reduces flood crests on the Peace, Slave and Mackenzie rivers as far downstream as Fort Good Hope . This has made the Peace Valley more suitable for farming, but has had significant impacts on downstream wildlife and riparian communities. The more stable annual flow slows down the spread of essential nutrients which builds up in

3783-472: The Holikachuks were in a position to borrow the Gwich'in contraction and to conflate its meaning with the meaning of Kuig-pak [River-big], which is the Yup'ik name for the same river. For that reason, the documentary evidence suggests that the Holikachuks had borrowed the contraction Ųųg Han [White Water River] from Gwich'in, and erroneously assumed that this contraction had the same literal meaning as

3880-526: The Liard River, it is 6,769 m /s (239,000 cu ft/s). At Norman Wells it is 8,446 m /s (298,300 cu ft/s), and at the Arctic Red confluence it is 8,926 m /s (315,200 cu ft/s). Mackenzie monthly mean discharge at Arctic Red River (m /s) As recently as the last glacial maximum about 30,000 years ago, the majority of northern Canada was buried under

3977-445: The Mackenzie River drainage basin encompasses nearly 20 percent of Canada. About 980,000 km (380,000 sq mi), or 54 percent of the basin, lies above Great Slave Lake. Permafrost underlies about three-quarters of the watershed, reaching up to 100 m (330 ft) deep in the Mackenzie Delta. As a whole, the Mackenzie basin receives only meager to moderate rainfall, averaging 410 millimetres (16 in) over

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4074-581: The Mackenzie River. Fort Providence lost 20 percent of its population, and some smaller villages and camps were completely wiped out. Steamboat service on the Mackenzie River began in the 1880s, and the number of vessels surged in the early 1900s as the Klondike Gold Rush brought a wave of prospectors to the Yukon. The Mackenzie River was one of the main routes into the northern interior, with sternwheelers transporting passengers, domestic supplies and industrial goods from as far upstream as

4171-498: The Mackenzie basin connects Norman Wells with Zama City , Alberta. Norman Wells was the main oil-producing area on the Mackenzie River until the 1970s, when new oil fields were discovered further north in the Mackenzie delta and the surrounding coastline. As of 2016, there were an estimated 166 billion barrels of oil reserves in this region. There is a proposal for a Mackenzie Valley Pipeline , which has not been built due to environmental concerns and falling oil and gas prices. During

4268-440: The Mackenzie is scant, despite the efforts of many researchers. Many archaeological sites have probably been destroyed by flooding, freeze-thaw and erosion. The Inuvialuit , Gwich'in and other Indigenous peoples have lived along the river for thousands of years; however, the oldest known evidence of continuous occupation stretches back only about 1300–1400 years, at the Gwich'in community of Tsiigehtchic . The Mackenzie provided

4365-556: The Mackenzie watershed is unbroken wilderness and human activities have little influence on the overall water quality, although there are some localized impacts. Some parts of the Mackenzie basin are rich in natural resources – oil and gas in the Northwest Territories and in central Alberta , lumber in the Peace River headwaters, uranium in Saskatchewan, gold and zinc in the Great Slave Lake area and tungsten in

4462-620: The Mountain River the Mackenzie flows due north until reaching The Ramparts , a limestone gorge barely 500 metres (1,600 ft) wide and up to 45 metres (148 ft) deep. Below The Ramparts is the village of Fort Good Hope , where the Mackenzie turns northwest again, soon crossing the Arctic Circle . The Mackenzie here flows slightly lower in elevation than the surrounding tundra , as a braided river between low bluffs about 3 to 5 km (1.9 to 3.1 mi) apart. It receives

4559-567: The Yukon River. The contraction is Ųųg Han , if the /ųų/ remains nasalized , or Yuk Han , if there is no vowel nasalization. In the 1840s, different tribes had different opinions as to the literal meaning of Yukon . In 1843, the Holikachuks had told the Russian-American Company that their name for the river was Yukkhana and that this name meant big river . However, Yukkhana does not literally correspond to

4656-557: The Yukon include set gillnets , drift nets , dip nets , and fish wheels . The preference of certain gear is largely dependent on the river's varied characteristics in different areas. Some parts of the river do not have eddies to make set-nets successful, whereas in other places the tributaries are small enough to make drifting impractical. Over the last 20 years salmon recruitment, the number of returning adults, has taken several shocks. The late 1980s, 1990s, and 2000s have been marked by radically reduced runs for various salmon species. In

4753-399: The Yukon. As of 2003 there were two operational gold mines in Yellowknife, and many more abandoned mines dot the region. Communities along the Mackenzie River depend on subsistence fishing, although there is also some commercial fishing on the river. Agriculture in the Mackenzie River basin is mainly concentrated in the Peace and Athabasca valleys to the south. The valley of the former river

4850-404: The basin, none of them endemic . The Mackenzie River has a similar range of fish fauna to the Mississippi River system. It is believed that the two river systems were connected during the Ice Ages by meltwater lakes and channels, allowing fish in the two rivers to interbreed. Fish in the Mackenzie River proper include the northern pike , several minnow species, and lake whitefish . Fish in

4947-577: The border. The agreement is implemented through the Yukon River Panel, an international body of 12 members, equal-parts American and Canadian, that advises managers of Yukon River fisheries concerning restoration, conservation, and coordinated management. Tribal organizations such as the Association of Village Council Presidents (AVCP), Council of Athabascan Tribal Governments (CATG), and Tanana Chiefs Conference (TCC) work to sustain Yukon River salmon to promote healthy people, cultures, and communities. The main river and tributaries are (sorted in order from

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5044-419: The company. Since then, Discovery II has been used on a regular basis to augment the passenger capacity of Discovery III on regular tours, as well as for special tours and charters. Yukon River The Yukon River is a major watercourse of northwestern North America. From its source in British Columbia , it flows through Canada's territory of Yukon (itself named after the river). The lower half of

5141-412: The corresponding Yup'ik name Kuig-pak [River-big]. The Lewes River is the former name of the upper course of the Yukon, from Marsh Lake to the confluence of the Pelly River at Fort Selkirk . The generally accepted source of the Yukon River is the Llewellyn Glacier at the southern end of Atlin Lake in British Columbia . Others suggest that the source is Lake Lindeman at the northern end of

5238-455: The current, with an estimated 35–50% bound for Canada. As a result, Chinook salmon are noted for their especially rich and fatty meat and are the priciest of all Pacific salmon species. The villages along the Yukon have historically relied on and continue to rely on salmon for their cultural, subsistence, and commercial needs. Salmon are traditionally dried, smoked, and frozen for both human and sled dog consumption. Common methods of fishing on

5335-549: The eastern and southern edges of the basin; these include uranium , gold , lead , and zinc . Agriculture remains prevalent along the south, particularly in the Peace River area. Various tributaries and headwaters of the river have been developed for hydroelectricity production, flood control and irrigation. Through its many tributaries, the Mackenzie River basin covers portions of five Canadian provinces and territories – British Columbia (BC), Alberta , Saskatchewan , Yukon , and Northwest Territories. Thutade Lake , in

5432-425: The effects of climate change on ocean food-supply & disease prevalence in returning adults, the methods of fishing used on the river, and the effects of the Bering Sea Pollock trawl fleet on food supply and salmon bycatch. In 2010, the Alaska Department of Fish & Game's Board of Fisheries issued the first-ever restriction for net mesh size on the Yukon, reducing it to 7.5 inches (190 mm). In 2021,

5529-498: The enormous continental Laurentide Ice Sheet . The tremendous erosive powers of the Laurentide and its predecessors, at maximum extent, completely buried what is now the Mackenzie watershed under thousands of metres of ice and flattened the eastern portions of the watershed. When the ice sheet receded for the last time, it left a 1,100 km (680 mi) long proglacial lake , Lake McConnell , of which Great Bear, Great Slave and Athabasca Lakes are remnants. Today's Mackenzie River

5626-423: The entire basin, though mountain areas experience much higher precipitation, and areas near and north of the Arctic Circle receive much lower precipitation. The Mackenzie drainage basin is bordered by multiple major North American watersheds. Much of the western edge of the Mackenzie basin runs along the Continental Divide . The divide separates the Mackenzie watershed from that of the Yukon River , which flows to

5723-457: The frozen river during the winter. Plans to build a permanent bridge were announced in March 2004, although they are currently on hold because bids came in much higher than budgeted. There are also two pedestrian-only bridges in Whitehorse, as well as a dam across the river and a hydroelectric generating station. The construction of the dam flooded the White Horse Rapids , which gave the city its name, and created Schwatka Lake . Transportation

5820-527: The government-owned Marine Transportation Services . In 2016, Northern Transportation Company went bankrupt, and its assets were bought by the government of Northwest Territories. Barge traffic travels the entire length of the Mackenzie in long "trains" of up to fifteen shallow-draft vessels pulled by tugboats . Goods are shipped as far as the port of Tuktoyaktuk on the eastern end of the Mackenzie Delta, where they are transferred to oceangoing vessels and delivered to communities along Canada's Arctic coast and

5917-420: The ice retreated, the Mackenzie system was captured to lower elevations in the northwest, establishing the present flow direction to the Arctic. Fluvial deposits and other erosional evidence indicate that around the end of the Pleistocene , about 13,000 years ago, the Mackenzie channel was scoured by one or more massive glacial lake outburst floods unleashed from Lake Agassiz , formed by melting ice west of

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6014-449: The ice-free season, the Mackenzie is a major transportation link through the vast wilderness of northern Canada, linking the many isolated communities along its course. Wide, calm sections of the river are frequently used to land seaplanes in the ice-free season. Canada's northernmost major railhead is located at the town of Hay River , on the south shore of Great Slave Lake. Goods shipped there by train and truck are loaded onto barges of

6111-419: The lake to rise, and the excess water can only flow out after the rivers have receded. The same phenomenon occurs at Great Slave Lake, which naturally regulates the flow from the Slave River into the Mackenzie. There are river gauges at several upstream points along the Mackenzie River. The average flow rate at the outlet of Great Slave Lake is 4,269 m /s (150,800 cu ft/s). At Fort Simpson, below

6208-442: The largest lakes in North America. By both volume and surface area, Great Bear Lake is the biggest in the watershed and third largest on the continent, with a surface area of 31,153 km (12,028 sq mi) and a volume of 2,236 km (536 cu mi). Great Slave Lake is slightly smaller, with an area of 28,568 km (11,030 sq mi) and containing 2,088 km (501 cu mi) of water, although it

6305-487: The major route into Canada's northern interior for European explorers as early as the late 18th century. Scottish explorer Alexander Mackenzie travelled the river in the hope it would lead to the Pacific Ocean , but instead reached its mouth on the Arctic Ocean on 14 July 1789. There is a story, likely apocryphal, that he named it "Disappointment River", but eventually it was named after him. No European reached its mouth again until Sir John Franklin on 16 August 1825 during

6402-404: The major route into Canada's northern interior for early European explorers. Economic development remains limited along the river. During the 19th century, fur trading became a lucrative business, but this was affected by harsh weather conditions. The discovery of oil at Norman Wells in the 1920s began a period of industrialization in the Mackenzie valley. Metallic minerals have been found along

6499-432: The massive cost and environmental impact. The Royal Canadian Mint honoured the 200th anniversary of the naming of the Mackenzie River with the issue of a silver commemorative dollar in 1989. In 1997, a cultural landscape along the section of the Mackenzie River at Tsiigehtchic was designated the Nagwichoonjik (Mackenzie River) National Historic Site of Canada due to its cultural, social and spiritual significance to

6596-455: The mid-twentieth century, more than 400,000 birds passed through during the spring and up to a million in autumn. Some 215 bird species in total have been catalogued in the delta, including species such as the whooping crane , peregrine falcon and bald eagle . The construction of the W.A.C. Bennett Dam on the Peace River has reduced the seasonal variations of water levels in the delta, causing damage to its ecosystem. Bird populations have seen

6693-411: The mine shut down in 1988, the railroad remains an important transportation link between the Mackenzie River waterway and the rest of Canada. In the 1950s the U.S. Army Corps of Engineers proposed the North American Water and Power Alliance (NAWAPA), a vast series of dams, tunnels and reservoirs designed to move 150 km (120,000,000 acre⋅ft) of water from northern Canada to southern Canada,

6790-486: The mouth heading upstream): tributary tributary (km) (km ) (m /s) (distributary) Teslin Period: 1971–2000 Mackenzie River (Period of data: 1984-2018)310 km /a (9,800 m /s) (Period of data: 1973-2011)10,300 m /s (360,000 cu ft/s) The Mackenzie River (French: Fleuve (de) Mackenzie ; Slavey : Deh-Cho [tèh tʃʰò], literally big river ; Inuvialuktun : Kuukpak [kuːkpɑk], literally great river )

6887-400: The north. Year round, the Mackenzie's outflow has a major stabilizing effect in the local climate above the Arctic Ocean with large amounts of warmer fresh water mixing with the cold seawater. The average flow rate at the mouth is 9,910 m /s (350,000 cu ft/s), the second largest in Canada after the St Lawrence , and the fourteenth largest in the world. About 60 percent of

6984-457: The numerous islands to the north. In winter, the frozen channel of the Mackenzie River, especially in the delta region, is used as an ice road , firm enough to support large trucks, although travel between northern communities is mostly by dog sleds and snowmobiles. Although the Mackenzie River is wide and deep, navigation is "notoriously difficult" due to the locations of sandbars and shallows changing from year to year. In some narrower parts of

7081-551: The oil due to poor construction. It only operated for thirteen months, shutting down in 1945. Much abandoned equipment remains along the corridor today; part of the pipeline route has been designated the Canol Heritage Trail . In 1964 the Mackenzie Northern Railway (now a subsidiary of CN ) reached the shore of Great Slave Lake, to serve the new Pine Point zinc mine near Hay River. Although

7178-505: The present-day Great Lakes . At its peak, Agassiz had a greater volume than all present-day freshwater lakes combined. This is believed to have disrupted currents in the Arctic Ocean and led to an abrupt 1,300-year-long cold temperature shift called the Younger Dryas . The Mackenzie carries a very large sediment load, transporting about 128 million tonnes each year to its delta. The Liard River alone accounts for 32 percent of

7275-539: The region. Beaver and muskrat populations were heavily depleted, especially in areas around and south of Great Slave Lake. Catholic missionary Henri Grollier founded missions at Fort Simpson, Fort Norman and Fort Good Hope between 1858 and 1859. During the late 19th century and early 20th century epidemics of introduced European diseases swept through Indigenous communities along the river, and thousands of native people lost their lives. One particularly severe influenza in 1928 killed as many as one in ten native people along

7372-544: The river continues westward through the U.S. state of Alaska . The river is 3,190 kilometres (1,980 mi) long and empties into the Bering Sea at the Yukon–Kuskokwim Delta . The average flow is 6,400–7,000 m /s (230,000–250,000 cu ft/s). The total drainage area is 854,700 km (330,000 sq mi), of which 323,800 km (125,000 sq mi) lies in Canada. The total area

7469-627: The river until the 1950s, when the Klondike Highway was completed. After the purchase of Alaska by the United States in 1867, the Alaska Commercial Company acquired the assets of the Russian-American Company and constructed several posts at various locations on the Yukon River. The Yukon River has a recent history of pollution from military installations, dumps, wastewater, and other sources. However,

7566-404: The river, barges must be uncoupled and towed one by one through hazardous stretches, despite attempts to widen and deepening the channel by blasting. Although there are no dams along the main stem of the Mackenzie, many of its tributaries and headwaters have been developed for hydroelectricity production, flood control and irrigation. The W.A.C. Bennett and Peace Canyon hydroelectric dams on

7663-541: The runoff from the northern Yukon, joins in the delta at a point northeast of Fort McPherson . Below there, the Mackenzie diverges into several large channels with the largest heading north-northeast, emptying into the Beaufort Sea west of Tuktoyaktuk . The Mackenzie Delta contains a logjam with 400,000 caches of wood, which stores 3.4 million tons of carbon , equivalent to a year's emissions from 2.5 million cars. At 1,805,000 km (697,000 sq mi),

7760-514: The settlement of Yellowknife and the opening of several mines in the area. By the 1940s steamboats had been replaced by modern gas and diesel-powered craft, which continue to serve the river today. During World War II oil pumped in Norman Wells was shipped to Fairbanks , Alaska via the 1,000-kilometre (620 mi) Canol pipeline . The pipeline was considered a "fiasco", going five times over budget and losing as much as 20 percent of

7857-464: The southern half of the watershed are genetically isolated from those of the northern half due to large rapids on the Slave River preventing fish from swimming upstream. Migratory birds use the three major deltas in the Mackenzie River basin – the Mackenzie Delta and the inland Slave and Peace-Athabasca Deltas – as resting and breeding areas. The latter is located at the convergence of four major North American migratory routes, or flyways. As recently as

7954-478: The spring, the difference in discharge between the two halves of the watershed becomes even more marked. While large amounts of snow and glacial melt dramatically drive up water levels in the Mackenzie's western tributaries, large lakes to the east retard springtime discharges. Spring floods from the Peace-Athabasca system are significantly slowed by the delta area at the western end of Lake Athabasca causing

8051-494: The summer melt – which does not fully mix with the clear water in the Mackenzie for almost 500 km (310 mi) downstream, with the resulting phenomenon of a clear current on the east bank and muddy water on the west bank. The river continues west-northwest until its confluence with the North Nahanni River , where it turns north towards the Arctic. It flows through open taiga with its wide valley bounded, on

8148-446: The summer of 2023, the U.S. Fish and Wildlife Service counted 58,500 Chinook salmon, the second lowest season on record. The United States Department of Commerce issued a Federal Disaster Declaration for the 2008 and 2009 Commercial Chinook Yukon River fisheries, calling for the complete closure of commercial fishing along with restrictions on subsistence fishing. The root cause of these poor returns remains debated, with questions about

8245-562: The summer, and used as an ice bridge in the winter for traffic along the Yellowknife Highway . In 2012 the Deh Cho Bridge was completed at a point about 10 km (6.2 mi) upstream, providing a safer permanent crossing. It is the only bridge across the main stem of the Mackenzie. West of Fort Providence the Mackenzie widens considerably, resembling a shallow, swampy lake more than a river; one large widening here

8342-402: The taiga consists of black spruce , aspen and poplar forest. In the north, the river's shores are lined with sparse vegetation like dwarf birch and willows , as well as extensive areas of muskeg and peat bogs . South of Great Slave Lake, there are much larger reaches of temperate and alpine forest, prairie, and fertile floodplain and riparian habitat. There are 53 fish species in

8439-472: The total river flow into the Arctic Ocean. The river is frozen for most of the year, with the ice typically breaking up by early to mid-May in the south, and late May-early June in the north. Ice breaks up earlier on the tributaries, sometimes causing ice jams and flooding where they meet the Mackenzie. In the middle of the larger lakes, such as Great Slave, ice can persist as late as mid-June. The river typically freezes by late October or November, starting in

8536-487: The total, and the Peel River about 20 percent. Essentially all of the sediment is contributed by areas downstream of Fort Providence, since upstream sediment is trapped in Great Slave Lake. The Mackenzie River's watershed is considered one of the largest and most intact ecosystems in North America, especially the northern half. Approximately 63% of the drainage basin, or 1,137,000 km (439,000 sq mi),

8633-560: The upper Peace River were completed in 1968 and 1980 by BC Hydro . They have a combined capacity of more than 3,600 megawatts (MW). The reservoir of W.A.C. Bennett, Williston Lake , is the largest body of fresh water in BC and the ninth largest man-made lake in the world, with a volume of 70.3 km (57,000,000 acre⋅ft). Other smaller hydroelectric plants are located along the Snare and Taltson River tributaries, providing power to mines in

8730-537: The village fishers that have traditionally managed these resources, enabling communication between fishers and fishery managers, and helping to preserve the ecological integrity of salmon runs and local cultures' Traditional Ecological Knowledge In March 2001, the U.S. & Canadian governments passed the Yukon River Salmon Agreement to better manage an internationally shared resource and ensure that more Canadian-originated salmon return across

8827-491: The water comes from the western half of the basin, which includes the Rocky, Selwyn , and Mackenzie mountain ranges out of which spring major tributaries such as the Peace and Liard Rivers, which contribute 23 and 27 percent of the total flow, respectively. In contrast the eastern half, despite being dominated by marshland and large lakes, provides only about 25 percent of the Mackenzie's discharge. During peak flow in

8924-755: The west, by the Mackenzie Mountains and to the east by low hills of the Canadian Shield . This mostly uninhabited area is called the Mackenzie Lowlands; although partly forested, it is mostly covered by large areas of muskeg , swamps and many small lakes. A number of major tributaries join from the west, including the Root River, Redstone River and Keele River . Below the Keele River, the Mackenzie River flows north along

9021-590: The western United States and Mexico. The system would involve building massive dams on the Liard, Mackenzie, Peace, Columbia , and Fraser river systems and pumping water into a 650 km (400 mi) long reservoir in the Rocky Mountain Trench . The water would then flow by gravity to irrigate more than 220,000 km (85,000 sq mi) in the three countries and generate more than 50,000 MW of surplus energy. The projects were never built due to

9118-698: The western base of the Franklin Mountains before turning northwest, and receives the Great Bear River , the outflow of Great Bear Lake at Tulita . The Mackenzie widens considerably to about 6 to 7 km (3.7 to 4.3 mi) at Norman Wells , a major center of oil production. There is a narrows at the Mountain River confluence called the Sans Sault Rapids , where the Mackenzie falls about 6 metres (20 ft). Below

9215-446: The world . The ultimate source of the Mackenzie River is Thutade Lake , in the Northern Interior of British Columbia . The Mackenzie valley is believed to have been the path taken by prehistoric peoples during the initial human migration from Asia to North America over 10,000 years ago, despite sparse evidence. The Inuvialuit , Gwich'in and other Indigenous peoples lived along the river for thousands of years. The river provided

9312-500: The world. Each year Chinook , coho , and chum salmon return to their terminal streams in Alaska, the Yukon Territory , and British Columbia. As salmon do not eat during their spawning migration, Yukon River salmon must have great reserves of fat and energy to fuel their thousands-mile-long journey. The Chinook, which arrive at the mouth of the Yukon River in early June, have the longest journey – as many as 2,000 miles against

9409-548: Was first discovered by Imperial Oil in 1971–1972. As of 2001, approximately 400,000 people lived in the Mackenzie River basin – representing only one percent of Canada's population. Ninety percent of the population lived in the Peace and Athabasca River basins, mostly in Alberta. The cold northern permafrost regions beyond the Arctic Circle are very sparsely populated, mainly by Indigenous peoples . Most of

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