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Doig River
The Doig River is a river in Alberta and northern British Columbia, Canada. It originates on the northern fringes of Peace River Country in northern Alberta, south of the Chinchaga Wildland Park, in the Halverson Ridge of the Clear Hills, then flows westwards into British Columbia. It empties into the Beatton River, a tributary of the Peace River, at an elevation of . Tributaries include the Square Creek, Betts Creek and Mearon Creek in Alberta; Adskwatim Creek, Osborn River, La Guarde Creek, and Siphon Creek in British Columbia. The Indigenous community of Doig River is located in British Columbia along the river on reserve No 206, based on Treaty No. 8 and signed by the Beaver community as the last tribe in May 1900. There were 140 inhabitants in 2001, 125 thereof Indians. 50% of the inhabitants were fluent in the Athabascan (Beaver) language; 28,6% of the population spoke Beaver as their mother-tongue. The Doig Airport is located at Doig, Alberta. The Doig Formation, ...
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Clear Hills County
Clear Hills County is a municipal district in north western Alberta, Canada. It is located in Census Division 17. In 1950, the massive Chinchaga fire burned through much of the region. On January 1, 2006, the name was changed from ''Municipal District of Clear Hills No. 21'' to Clear Hills County.Municipal Profile
- Alberta Municipal Affairs


Geography


Communities and localities

Athabascan
Athabaskan (also spelled ''Athabascan'', ''Athapaskan'' or ''Athapascan'', and also known as Dene) is a large family of indigenous languages of North America, located in western North America in three areal language groups: Northern, Pacific Coast and Southern (or Apachean). Kari and Potter (2010:10) place the total territory of the 53 Athabaskan languages at . Chipewyan is spoken over the largest area of any North American native language, while Navajo is spoken by the largest number of people of any native language north of Mexico. ''Athebaskan '' is a version of a Cree name for Lake Athabasca ( crm, Āðapāskāw, script=Latn 'herethere are reeds one after another'), in Canada. Cree is one of the Algonquian languages and therefore not itself an Athabaskan language. The name was assigned by Albert Gallatin in his 1836 (written 1826) classification of the languages of North America. He acknowledged that it was his choice to use that name for the language family and its asso ...
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List Of Rivers Of British Columbia
The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes that are "in-line" connecting upper tributaries of listed rivers, or at their heads. Arctic drainage Arctic Ocean via Mackenzie River drainage :''(NB Liard tributaries on Yukon side of border omitted)'' Liard River watershed *Liard River ** Petiewewtot River **Fort Nelson River ***Sahtaneh River ****Snake River *** Muskwa River **** Prophet River ***** Minaker River *****Besa River ****Tetsa River ****Chischa River ****Tuchodi River *** Sikanni Chief River **** Buckinghorse River *** Fontas River **Dunedin River ** Beaver River **Toad River *** West Toad River *** Racing River *** Schipa River ** Grayling River ** Trout River **Vents River ** Smith River ** Coal River ** Rabbit River *** Gundahoo River **Kechika River *** Red River ***Turna ...
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List Of Rivers Of Alberta
Alberta's rivers flow towards three different bodies of water, the Arctic Ocean, the Hudson Bay and the Gulf of Mexico. Alberta is located immediately east of the continental divide, so no rivers from Alberta reach the Pacific Ocean. List of rivers in Alberta The north of the province is drained towards the Arctic Ocean, and the northern rivers have comparatively higher discharge rates than the southern ones, that flow through a drier area. Most of Alberta's southern half has waters flowing toward the Hudson Bay, the only exception being the Milk River and its tributaries, that flow south through the Missouri and Mississippi River to the Gulf of Mexico. Arctic Ocean watershed Albertan rivers in the Arctic Ocean watershed are drained through Great Slave Lake and Mackenzie River, except for Petitot River which is drained through Liard River directly into the Mackenzie River, thus bypassing the Great Slave Lake. *Athabasca River ** Chaba River ** Sunwapta River ** Whirlpoo ...
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Western Canadian Sedimentary Basin
The Western Canadian Sedimentary Basin (WCSB) underlies of Western Canada including southwestern Manitoba, southern Saskatchewan, Alberta, northeastern British Columbia and the southwest corner of the Northwest Territories. This vast sedimentary basin consists of a massive wedge of sedimentary rock extending from the Rocky Mountains in the west to the Canadian Shield in the east. This wedge is about thick under the Rocky Mountains, but thins to zero at its eastern margins. The WCSB contains one of the world's largest reserves of petroleum and natural gas and supplies much of the North American market, producing more than per day of gas in 2000. It also has huge reserves of coal. Of the provinces and territories within the WCSB, Alberta has most of the oil and gas reserves and almost all of the oil sands. Conventional oil The WCSB is considered a mature area for exploration of petroleum and recent development has tended toward natural gas and oil sands rather than conventional ...
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Triassic
The Triassic ( ) is a geologic period and system (stratigraphy), system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Year#Abbreviations yr and ya, Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic, Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vert ...
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Doig Formation
The Doig Formation is a geologic formation of middle Triassic age in the Western Canadian Sedimentary Basin. It takes the name from Doig River, a tributary of the Beatton River, and was first described in the Texaco N.F.A. Buick Creek No. 7 well (located north-west of Fort St. John, east of the Alaska Highway) by J.H. Armitage in 1962. . Lithology The Doig Formation is composed of fine grained, grey argillaceous siltstone and dark calcareous shale. Phosphate nodules occur at the base of the formation. Anomalously thicker, porous sandstone channels and bars are present locally in the upper units of the formation. The formation has provided fossils of various species of conodonts; '' Magnigondolella alexanderi'', '' M. cyri'', '' M. julii'', '' M. nebuchadnezzari'', '' M. salomae'', '' Neogondolella curva'', '' N. hastata'', '' N. panlaurentia'' and '' N. ex gr. shoshonensis''. Distribution The Doig Formation reaches a maximum thickness of in the Canadian Rockies footh ...
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Doig, Alberta
Doig is an unincorporated community in northern Alberta, Canada. It is located in Clear Hills County, in a muskeg and boreal forest landscape. The Doig Airport is located here. It was named after the Doig River, a tributary of Beatton River. The middle Triassic bituminous Doig Formation was named after this place. Clear Hills County {{NorthernAlberta-geo-stub ...
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Doig Airport
Doig Airport is a remote forest fire suppression airfield located in northwestern Alberta, Canada. "Doig" is just the name of the airfield's location, named for the Doig River; there is no community with that name. The airfield is located on the Halveston Ridge of the Clear Hills Clear Hills County is a municipal district in north western Alberta, Canada. It is located in Census Division 17. In 1950, the massive Chinchaga fire burned through much of the region. On January 1, 2006, the name was changed from ''Municip ..., north of the Doig River. References External linksPage about this airporton COPA's ''Places to Fly'' airport directory Registered aerodromes in Alberta Clear Hills County {{Alberta-airport-stub ...
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Beaver
Beavers are large, semiaquatic rodents in the genus ''Castor'' native to the temperate Northern Hemisphere. There are two extant species: the North American beaver (''Castor canadensis'') and the Eurasian beaver (''C. fiber''). Beavers are the second-largest living rodents after the capybaras. They have stout bodies with large heads, long chisel-like incisors, brown or gray fur, hand-like front feet, webbed back feet and flat, scaly tails. The two species differ in the shape of the skull and tail and fur color. Beavers can be found in a number of freshwater habitats, such as rivers, streams, lakes and ponds. They are herbivorous, consuming tree bark, aquatic plants, grasses and sedges. Beavers build dams and lodges using tree branches, vegetation, rocks and mud; they chew down trees for building material. Dams impound water and lodges serve as shelters. Their infrastructure creates wetlands used by many other species, and because of their effect on other organisms in ...
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Beatton River
The Beatton River is a tributary of the Peace River, flowing generally east, then south through north-eastern British Columbia, Canada. The river rises at Pink Mountain, about west of the Alaska Highway hamlet of the same name, and flows generally east, then south, draining into the Peace River just downstream of Fort St. John. The river meanders mostly through the boreal forest and muskeg of the Peace Plain. Its major tributaries are the Doig and Blueberry Rivers. The area around the river is the homeland of the Dane-zaa or Beaver First Nation. Archaeologists have found evidence of human habitation in the area dating back at least 10,000 years. The mouth of the Beatton River was the location of a Northwest Company fort established in 1806. Modern-day British Columbia's first European settlement was fur trading Rocky Mountain Fort, established in 1794 at the mouth of the Moberly River near the present Fort St. John. The river became an important route for First Nations pe ...
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Treaty 8 Tribal Association
Treaty 8 Tribal Association (T8TA) is an association of six of the eight Peace River Country First Nations bands who are signatories to Treaty 8 in northeastern British Columbia. They have joined together in an effort to negotiate with British Columbia and Canada outside the British Columbia Treaty Process. Incorporated in 1982 under the ''BC Societies Act'', T8TA is primarily funded by the federal Department of Crown–Indigenous Relations and Northern Affairs. Members *Doig River First Nation – Northeast of Fort St. John, BC * Fort Nelson First Nation – Fort Nelson, BC *Halfway River First Nation – Northwest of Fort St. John, BC * Prophet River First Nation – South of Fort Nelson, BC *Saulteau First Nations – Chetwynd, BC *West Moberly First Nations – Peace River Country in northern BC Treaty process Blueberry River First Nations retained lawyer and academic Murray Rankin who successfully negotiated the first Economic Benefits Agreement relating to natural re ...
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