(Period of data: 1984-2018)310 km /a (9,800 m /s)
88-810: The Keele River is a tributary of the Mackenzie River , about 410 kilometres (250 mi) long, in the western part of the Canadian Northwest Territories . Flowing in a generally northeast direction, it drains a sparsely populated, rugged area of the Mackenzie Mountains . The Keele River originates in a small, unnamed lake near the border of the Northwest Territories and the Yukon , approximately 25 kilometres (16 mi) south of Macmillan Pass, which
176-544: A guided expedition, and intermediate paddlers who wish to challenge it themselves. Several outfitting and guiding companies offer guided tours down the Natla/Keele river system during all months of the summer, as well as outfitting services. Trips usually depart Norman Wells or Fort Simpson by floatplane and land on the river at the Natla-Keele confluence. Trip length is usually between 10 and 14 days; however, it
264-802: A modified Latin script , with some using Canadian Aboriginal syllabics . In their own languages, these languages are referred to as: Sahtúgot’įné Yatı̨́ (spoken by the Sahtu Dene ), K’ashógot’įne Goxedǝ́ (the Hare Dene dialect) and Shíhgot’įne Yatı̨́ (the Mountain dialect) in the North, and Dené Dháh (primarily by the Dene Tha' in Alberta ), Dene Yatıé or Dene Zhatıé in the South. North Slavey
352-539: A separate phoneme. Prenasalized stops /ᵐb, ⁿd/ may appear in Slavey proper. The most pronounced difference is however the realization of a series of consonants that varies greatly in their place of articulation: In Slavey proper, these are dental affricates and fricatives; comparative Athabaskan work reveals this to be the oldest sound value. Mountain has labials, with the voiceless stop coinciding with pre-existing /p/ . Bearlake has labialized velars, but has lenited
440-528: 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
528-478: A very specific morpheme order in the verb in which the stem must come last. The morpheme order is shown in the following chart. A Slavey verb must minimally have positions 13 and 14 to be proper. Here are some examples: Slavey marks gender by means of prefixation on the verb theme. There are three different genders, one of which is unmarked; the other two are marked by prefixes [go-] and [de-] . However, only certain verb themes allow gender prefixes. [go-]
616-543: 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
704-838: 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
792-464: Is based largely on the way each one pronounces the old Proto-Athapaskan sounds *dz *ts *ts’ *s and *z. The consonant inventories in the dialects of Slavey differ considerably. The table above lists the 30 consonants common to most or all varieties. Hare lacks aspirated affricates (on red background), which have lenited into fricatives, whereas Mountain lacks /w/ (on blue). In addition, for some speakers of Hare, an alveolar flap /ɾ/ has developed into
880-649: 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
968-418: Is due to a perfect combination of spectacular rugged mountain scenery, excellent fishing and wildlife viewing and fun but challenging class 2+ whitewater with no portages . Swift currents, rapids and aquamarine glacial water in a wilderness setting hundreds of kilometres from the nearest road mean that this river offers a thrill to all who paddle it. The Keele is suitable for beginner canoeists when paired with
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#17327661618681056-524: Is feasible to have a longer trip by pairing the Keele with the Natla river. (Natla is a class 3+ river, and therefore is an experts-only trip). The upper Keele River above the confluence with the Natla is also a class 2-3 navigable waterway, but suffers from accessibility issues, as there are no lakes for a float plane to land on at the headwaters of the river. Paddlers looking to go down this section usually access
1144-526: 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
1232-426: 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
1320-539: 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
1408-510: Is marked with an acute accent, and low tone is unmarked. Tones are both lexical and grammatical. Lexical: /ɡáh/ 'along' vs. /ɡàh/ 'rabbit' Slavey morphemes have underlying syllable structures in the stems: CV, CVC, CVnC, V, and VC. The prefixes of the stem occur as Cv, CVC, VC, CV, and C. Slavey alphabet (1973) Tone is indicated with an acute accent and the ogonek indicates nasalization. North Slavey alphabet South Slavey alphabet Slavey, like many Athabascan languages, has
1496-562: 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
1584-678: 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
1672-556: Is spoken by the Sahtu (North Slavey) people in the Mackenzie District along the middle Mackenzie River from Tulita (Fort Norman) north, around Great Bear Lake , and in the Mackenzie Mountains of the Canadian territory of Northwest Territories . The dialect has around 800 speakers. Northern Slavey is an amalgamation of three separate dialects : South Slavey ( ᑌᓀ ᒐ Dené Dháh , Dene Yatıé or Dene Zhatıé )
1760-836: Is spoken by the Slavey people, who were also known as Dehghaot'ine, Deh Cho, Etchareottine - "People Dwelling in the Shelter", in the region of Great Slave Lake , upper Mackenzie River ( Deh Cho - "Big River") and its drainage, in the District of Mackenzie, northeast Alberta , and northwest British Columbia . Some communities are bilingual, with the children learning Slavey at home and English when they enter school. Still other communities are monolingual in Slavey The dialect has around 1,000 speakers. Alternative names: Slavi, Slave, Dené, Mackenzian The division of Slavey dialects
1848-733: Is the terminus of the drivable section of the North CANOL Road . The river begins its journey by flowing northwest through the alpine tundra area known as the Mackenzie Mountain Barrens, joining the Tsichu and Intga Rivers along the way. It then drops off the alpine plateau and begins its long descent to the Mackenzie River, tumbling gradually down into the dramatic Backbone Ranges of the Mackenzie Mountains. Approximately 100 kilometres (62 mi) from
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#17327661618681936-492: Is used for nouns which mark location in either time or space. Some examples of these areal nouns are house (ko̜̒e̒), land (de̒h), river (deh), and winder (xay). The gender pronoun can be a direct object, an oblique object or a possessor. kú̜e̒ house go detl’e̒h 3SG .paints.area kú̜e̒ go detl’e̒h house 3SG.paints.area 'S/he is painting the house.' ko̜̒e̒ house go cha area.in shelter ko̜̒e̒ go cha {} house area.in shelter 'in
2024-592: 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
2112-618: 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
2200-538: 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
2288-888: 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
2376-762: 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
2464-588: 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
2552-649: 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
2640-596: The Redstone River and 50 kilometres (31 mi) south-southeast of Tulita . People have inhabited the mountainous area surrounding the Keele River for at least 11,000 years. The Dene name for the Keele River is Begádeé, which translates to "Winding River". The river was used extensively as a trade route for some tribes of the Mountain Dene people. After spending the summer hunting and trading along
2728-568: 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
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2816-758: 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
2904-455: 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
2992-642: The 1800s. Come spring, they would return to the mountains once again on foot. After signing Treaty 11 (regarding the transfer of lands in the Yukon to the federal government for purposes of oil exploration) with King George V in 1921, the Dene no longer went to the Yukon Border area as frequently and as a result the Keele was also less travelled. The Keele also has been known as the Gravel River . The river
3080-453: 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
3168-503: 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
3256-579: 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
3344-460: The Keele through the class 3-4 Tischu River after landing on an air strip at Mile 222 of the Canol Road. Mackenzie River (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 )
3432-717: The Keele's source, the Natla River rushes into the Keele from the south and almost doubles the flow and size of the river. From the Natla Confluence, The Keele turns and snakes its way northward for 85 kilometres (53 mi) until it meets the Twitya River, its largest tributary, flowing in from the west. Just after the Twitya confluence, the Keele is deflected east around the Tigonankweine Range by
3520-526: 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
3608-445: 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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3696-513: 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
3784-498: 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
3872-440: 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
3960-422: 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
4048-494: 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
4136-399: 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
4224-400: The Yukon/NWT border the Mountain Dene, or shúhtagot'ıne, would build large moose skin boats, fill them with furs and goods and paddle down the Keele River to their winter camps along the Mackenzie River Valley. There they would trade these furs and goods for supplies to survive the long winter months with the Lowland Dene People and the Hudson Bay trading post after it was built at Fort Norman in
4312-404: 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
4400-549: 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
4488-498: 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
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#17327661618684576-423: 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
4664-406: The form of sediments, thus causing the river to become more polluted. Slavey language Slavey ( / ˈ s l eɪ v i / ; also Slave , Slavé ) is a group of Athabaskan languages and a dialect continuum spoken amongst the Dene peoples of Canada in the Northwest Territories – or central Denendeh – where it also has official status. The languages are primarily written using
4752-527: 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
4840-420: 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
4928-449: 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
5016-419: 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
5104-442: 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
5192-487: 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
5280-404: 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
5368-432: 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
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#17327661618685456-455: 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
5544-411: 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,
5632-400: 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
5720-457: 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
5808-401: 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
5896-443: 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
5984-539: 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
6072-404: 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
6160-480: 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),
6248-453: 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
6336-464: 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
6424-478: 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
6512-494: 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
6600-562: 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
6688-402: 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
6776-472: 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
6864-487: 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),
6952-491: The towering Mount Eduni Massif and continues in this direction until reaching the Mackenzie River. During this section, the Toochingkla River flows in from the south, before the Keele cuts between the spectacular Canyon and Redstone Ranges. It then leaves the mountains behind, becoming slow and braided, and receives Middle Creek from the south, merging into the Mackenzie some 13 kilometres (8.1 mi) downstream from
7040-560: 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
7128-537: The voiced fricative to coincide with pre-existing /w/ . The most complicated situation is found in Hare, where the plain stop is a labialized velar, the ejective member is replaced by a /ʔw/ sequence, the aspirated affricate has turned into a fricative /f/ , and both the voiceless and voiced fricatives have been lenited to /w/ . The following phonological and phonetic statements apply to all four dialects of Slavey. Slavey has two tones: In Slavey orthography, high tone
7216-491: 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
7304-625: 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
7392-590: 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
7480-698: 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
7568-446: 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
7656-548: 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
7744-646: Was named, as was the Keele Peak , for Joseph Keele, a member of the Geological Survey of Canada , who had surveyed the area in 1907–08, and descended the Keele River from its source to the Mackenzie. In recent years the Keele River, the less travelled cousin of the South Nahanni River , has become known as a world class destination for wilderness canoeing and rafting, seeing hundreds of people paddle down its lower section each summer. This
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