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Mackenzie River
The Mackenzie River (French: ; Slavey language, Slavey: ' [tèh tʃʰò], literally ''big river''; Inuvialuktun: ' [kuːkpɑk], literally ''great river'') is a river in the Canadian Canadian boreal forest, boreal forest and tundra. It forms, along with the Slave River, Slave, Peace River, Peace, and Finlay River, Finlay, the longest river system in Canada, and includes the second largest drainage basin of any North American river after the Mississippi River, 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 Provinces and territories of Canada, Canadian provinces and territories. The river's mainstem (hydrology), main stem is long, flowing north-northwest from Great Slave Lake into the Arctic Ocean, where it forms a large River delta, delta at its mouth. Its extensive watershed drains about 20 percent of Canada. It is t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Language
French ( or ) is a Romance languages, Romance language of the Indo-European languages, Indo-European family. Like all other Romance languages, it descended from the Vulgar Latin of the Roman Empire. French evolved from Northern Old Gallo-Romance, a descendant of the Latin spoken in Northern Gaul. Its closest relatives are the other langues d'oïl—languages historically spoken in northern France and in southern Belgium, which French (Francien language, Francien) largely supplanted. It was also substratum (linguistics), influenced by native Celtic languages of Northern Roman Gaul and by the Germanic languages, Germanic Frankish language of the post-Roman Franks, Frankish invaders. As a result of French and Belgian colonialism from the 16th century onward, it was introduced to new territories in the Americas, Africa, and Asia, and numerous French-based creole languages, most notably Haitian Creole, were established. A French-speaking person or nation may be referred to as Fra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inuvik, Northwest Territories
Inuvik (''place of man'') is the only town in the Inuvik Region, and the third largest community in Canada's Northwest Territories. Located in what is sometimes called the Beaufort Delta Region, it serves as the region's administrative and service centre. Inuvik is home to federal, territorial, and Indigenous government offices, along with a regional hospital and airport. Inuvik is located on the northern edge of a boreal forest just before it begins to transition to tundra. It is on the east side of the enormous Mackenzie River delta. The town lies within the Gwich'in Settlement Region and the Inuvialuit Settlement Region. History Inuvik was conceived in 1953 as a replacement administrative centre for the hamlet of Aklavik on the west of the Mackenzie Delta, as the latter was prone to flooding and had no room for expansion. Initially called "New Aklavik", it was renamed Inuvik in 1958. The school was built in 1959 and the hospital, government offices and staff residenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tundra
In physical geography, a tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. There are three regions and associated types of tundra: #Arctic, Arctic, Alpine tundra, Alpine, and #Antarctic, Antarctic. Tundra vegetation is composed of dwarf shrubs, Cyperaceae, sedges, Poaceae, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained greenhouse gases into the atmosphere, creating Climate change feedback, a feedback cycle t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Boreal Forest
Canada's boreal forest is a vast region comprising about one third of the circumpolar boreal forest that rings the Northern Hemisphere, mostly north of the 50th parallel. Other countries with boreal forest include Russia, which contains the majority; the United States in its northernmost state of Alaska; and the Scandinavian or Northern European countries (e.g. Sweden, Finland, Norway and small regions of Scotland). In Europe, the entire boreal forest is referred to as taiga, not just the northern fringe where it thins out near the tree line. The boreal region in Canada covers almost 60% of the country's land area. The Canadian boreal region spans the landscape from the most easterly part of the province of Newfoundland and Labrador to the border between the far northern Yukon and Alaska. The area is dominated by coniferous forests, particularly spruce, interspersed with vast wetlands, mostly bogs and fens. The boreal region of Canada includes eight ecozones. While the biodiv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Simpson
Fort Simpson (Slavey language: ''Łı́ı́dlı̨ı̨ Kų́ę́'' "place where rivers come together") is a village, the only one in the entire territory, in the Dehcho Region of the Northwest Territories, Canada. The community is located on an island at the confluence of the Mackenzie and Liard rivers. It is approximately west of Yellowknife. Both rivers were traditionally trade routes for the Hudson's Bay Company and the native Dene people of the area. Fort Simpson is the regional centre of the Dehcho and is the gateway to the scenic South Nahanni River and the Nahanni National Park Reserve. Fort Simpson can be reached by air, water and road and has full secondary and elementary school service. The Mackenzie Highway was extended to Fort Simpson in 1970-71. The central section of the community is on an island near the south bank of the Mackenzie River, but industrial areas and rural residential areas are located along the highway as far as the Fort Simpson Airport, jus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tsiigehtchic
Tsiigehtchic ( ; "mouth of the iron river"), officially the ''Hamlet of Tsiigehtchic'', is a Gwichʼin community located at the confluence of the Mackenzie River, Mackenzie and the Arctic Red Rivers, in the Inuvik Region of the Northwest Territories, Canada. The community was formerly known as ''Arctic Red River'', until 1 April 1994. The Gwichya Gwich'in First Nation is located in Tsiigehtchic. History Ancient history Archaeology and oral history indicate that the flats below Tsiigehtchic have been used for the past 1,400 years by the Gwichyaa Gwichʼin, for various activities which were both commercial and recreational. The Gwich’in name for the flats is Łèth T’urh Kak (“on the mud flats”). Late modern period and the first European contact The first European contact with the Gwichya Gwich’in occurred in the summer of 1789, just prior to the late modern period, when Alexander Mackenzie (explorer), Alexander Mackenzie reached the area with his party of explorer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Bear River
The Great Bear River, which drains the Great Bear Lake westward through marshes into the Mackenzie River, forms an important transportation link during its four ice-free months. It originates at south-west bay of the lake. The river has irregular meander pattern channel with average depth . Historic air photos show no evidence of bank erosion or channel migration in a 50-year period. The low discharge rate is due to small amount of precipitation in watershed area. Great Bear River contained open reaches that had melted out in place over 80 percent of its length in 1972 and 1974. The settlement of Tulita is located at the mouth of the river. Ecology Great Bear River hosts a number of aquatic species, with some of the most notable being Lake trout and Lake whitefish. Other animals regularly found in the Great Bear River include various fish species such as Arctic grayling, Burbot, Cisco (lake herring), Northern Pike, Nelma (inconnu), Walleye, Fourhorn sculpin, Slimy scul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peel River (Canada)
The Peel River (' in Gwich’in) is a tributary of the Mackenzie River in Yukon and the Northwest Territories in Canada. Its source is in the Ogilvie Mountains in central Yukon at the confluence of the Ogilvie River and Blackstone River. Its main tributaries are: *Ogilvie River *Blackstone River * Hart River * Wind River (Yukon) * Bonnet Plume River * Snake River (Yukon) The Peel River joins the Mackenzie in the Mackenzie Delta. However, a distributary of the Peel is the headwater for a channel that later collects distributaries of the Mackenzie. This means that a channel can be followed for a longer distance downriver until it, itself, disseminates into the shared delta. This arguably adds a greater length to the Peel River. The Dempster Highway crosses it at Fort McPherson, via a ferry during the summer months and an ice bridge during the winter. The Peel River is a wilderness river and Fort McPherson is the only community along its banks. The Yukon part of the Peel Water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Red River
The Arctic Red River is a tributary to the Mackenzie River in the Northwest Territories, Canada. In 1993 the river was designated as part of the Canadian Heritage Rivers System. It was also the name of a community on the Mackenzie where the river joins, now known as Tsiigehtchic. The Dempster Highway crosses the Mackenzie at this point. The Arctic Red River's headwaters are in the Mackenzie Mountains, from where it flows northwest to its confluence with the Mackenzie. The river flows through a deep canyon as it flows through the Peel Plateau. The Gwichʼin name for the river, ''Tsiigèhnjik'', translates as ''iron river''. The lower of the river are navigable by kayakers and canoers, without requiring portaging Portage or portaging ( CA: ; ) is the practice of carrying water craft or cargo over land, either around an obstacle in a river, or between two bodies of water. A path where items are regularly carried between bodies of water is also called a '' .... Measured a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keele River
The Keele River is a tributary of the Mackenzie River, about 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. Course The Keele River originates in a small, unnamed lake near the border of the Northwest Territories and the Yukon, approximately south of Macmillan Pass, which 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 from 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, T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liard River
The Liard River of the Boreal forest of Canada, North American boreal forest flows through Yukon, British Columbia and the Northwest Territories, Canada. Rising in the Saint Cyr Range of the Pelly Mountains in southeastern Yukon, it flows southeast through British Columbia, marking the northern end of the Rocky Mountains and then curving northeast back into Yukon and Northwest Territories, draining into the Mackenzie River at Fort Simpson, Northwest Territories. The river drains approximately of boreal forest and muskeg. Geography The river habitats are a subsection of the Lower Mackenzie Freshwater Ecoregion. The area around the river in Yukon is called the ''Liard River Valley'', and the Alaska Highway follows the river for part of its route. This surrounding area is also referred to as the ''Liard Plain'', and is a physiographic section of the larger Yukon–Tanana Uplands province, which in turn is part of the larger Intermontane Plateaus physiographic division. The Liard ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inuvik Region
The Inuvik Region or ''Beaufort Delta Region'' is one of List of regions of the Northwest Territories, five administrative regions in the Northwest Territories of Canada. According to Municipal and Community Affairs the region consists of eight communities with the regional office situated in Inuvik. Most of the communities are in the Beaufort Sea area and are a mixture of Inuit (mostly Inuvialuit) and First Nations in Canada, First Nations (mostly Gwichʼin). Formerly, there was also a Statistics Canada designated Census geographic units of Canada, census division named Inuvik Region, Northwest Territories (former census division), Inuvik Region, Northwest Territories, which was abolished in the 2011 Canadian census. The territorial extent of this census division was somewhat larger than the administrative region of the same name. Administrative Region communities The Inuvik Region administrative entity includes the following communities: Communities in the Inuvik Regio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
