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Toodoggone River
The Toodoggone River is a tributary of the Finlay River in the Northern Interior of British Columbia, Canada, flowing east into the upper reaches of the Finlay just south of the Fishing Lakes. At the head of the Toodoggone is Metsantan Pass, which is at the divide with the Stikine River basin and also on the spine of the Continental Divide. Name origin The name is an English adaptation of the older, more aboriginal name Thudegane, which is an adaptation of the Sekani language term ''Tuhda Ughane'', meaning "Two Brothers River" or "eagles nest".''Guzagi K'úgé'', published by Kaska Tribal Council, Watson Lake, 1997 See also *List of aboriginal placenames in Canada This list of place names in Canada of Indigenous origin contains Canadian places whose names originate from the words of the First Nations, Métis, or Inuit, collectively referred to as Indigenous Peoples. When possible the original word or phra ... References Rivers of the Omineca Mountains Northern Int ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny ...
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Finlay River
The Finlay River is a 402 km long river in north-central British Columbia flowing north and thence south from Thutade Lake in the Omineca Mountains to Williston Lake, the impounded waters of the Peace River formed by the completion of the W.A.C. Bennett Dam in 1968. Prior to this, the Finlay joined with the Parsnip River to form the Peace. The headwaters of the Finlay at Thutade Lake are considered the ultimate source of the Mackenzie River.''Atlas of Canada: Rivers of Canada'' page
Deserters Canyon is located just north of Williston Lake. The Finlay drains an area of 43,000 square kilometres and discharges at a mean rate of 600 cubic metres per second. Major tributaries of the Finla ...
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Metsantan Range
The Metsantan Range are a mountain range between the upper Stikine and the Finlay River drainages in northern British Columbia, Canada. It has an area of 1116 km2 and is a subrange of the Omineca Mountains which in turn form part of the Interior Mountains The Interior Mountains or Northern Interior Mountains are the semi-official names for an expansive collection of mountain ranges that comprises much of the northern half of the Canadian province of British Columbia and a large area of southern Yu ....Metsantan Range
in the Canadian Mountain Encyclopedia


See also

* Metsantan Pass * Metsantan Peak *
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British Columbia Interior
, settlement_type = Region of British Columbia , image_skyline = , nickname = "The Interior" , subdivision_type = Country , subdivision_name = , subdivision_type1 = Province , subdivision_name1 = , parts_type = Principal cities , p1 = Kelowna , p2 = Kamloops , p3 = Prince George , p4 = Vernon , p5 = Penticton , p6 = West Kelowna , p7 = Fort St. John , p8 = Cranbrook , area_blank1_title = 14 Districts , area_blank1_km2 = 669,648 , area_footnotes = , elevation_max_m = 4671 , elevation_min_m = 127 , elevation_max_footnotes = Mt. Fairweather , elevation_min_footnotes = Fraser River , population_as_of = 2016 , population = 961,155 , population_density_k ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces and ...
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Metsantan Pass
Metsantan Pass, , is a mountain pass in the Metsantan Range of the Omineca Mountains in the Northern Interior of British Columbia, Canada. It is located between Metsantan Lake, in the drainage basin of the Stikine River (NW) and the headwaters of the Toodoggone River (SE), a tributary of the Finlay River which is part of the Peace- Mackenzie River drainage area, and therefore is located along the Continental Divide A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, no .... See also * Metsantan Peak References Mountain passes of British Columbia Omineca Mountains Northern Interior of British Columbia Great Divide of North America {{BritishColumbiaInterior-geo-stub ...
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Stikine River
The Stikine River is a major river in northern British Columbia (BC), Canada and southeastern Alaska in the United States. It drains a large, remote upland area known as the Stikine Country east of the Coast Mountains. Flowing west and south for , it empties into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada.Lehner, B., Verdin, K., Jarvis, A. (2008)New global hydrography derived from spaceborne elevation data Eos, Transactions, AGU, 89(10): 93–94. Considered one of the last truly wild large rivers in BC, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys. Known as the "fastest-flowing navigable river in North America," the Stikine forms a natural waterway from northern interior British Columbia to the Pacific coast. The river has been used for millennia by indigenous peoples including the Tlingit an ...
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Continental Divide Of The Americas
The Continental Divide of the Americas (also known as the Great Divide, the Western Divide or simply the Continental Divide; ) is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and (in northern North America) Arctic oceans (including those that drain into the Gulf of Mexico, the Caribbean Sea and Hudson Bay). Although there are many other hydrological divides in the Americas, the Continental Divide is by far the most prominent of these because it tends to follow a line of high peaks along the main ranges of the Rocky Mountains and Andes, at a generally much higher elevation than the other hydrological divisions. Geography Beginning at the westernmost point of the Americas’ mainland ( Cape Prince of Wales, just south of the Arctic Circle), the Conti ...
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Sekani Language
The Sekani language or Tse’khene is a Northern Athabaskan language spoken by the Sekani people of north-central British Columbia, Canada. Phonology Consonants Sekani has 33 consonants: Vowels Tone Sekani has two tones: low and high. High tone is the more common tone. Syllables phonologically marked for tone are low. Nasalization Nasalization of vowels is phonemic and so changes the meaning. Sample words In the practical writing system used here for the Kwadacha Tsek'ene dialect, ''u'' represents the mid-central vowel, and ''oo'' represents the high back rounded vowel. An apostrophe represents a glottal stop, and an ogonek under a vowel represents nasalization. *dune man; person *tlįį dog *wudzįįh caribou *yus snow *chǫ rain *k’wus cloud *kwùn fire *’įįbèh summer *too water *mun lake *nun land *tselh axe *ʼukèʼ foot *’àtse my grandfather *’àtsǫǫ my grandmother *lhìghè’ one *lhèkwudut’e two *tadut’e three *dįįdut’e four *ǫ yes ...
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List Of Aboriginal Placenames In Canada
This list of place names in Canada of Indigenous origin contains Canadian places whose names originate from the words of the First Nations, Métis, or Inuit, collectively referred to as Indigenous Peoples. When possible the original word or phrase used by Indigenous Peoples is included, along with its generally believed meaning. Names listed are only those used in English or French, as many places have alternate names in the local native languages, e.g. Alkali Lake, British Columbia is ''Esket'' in the Shuswap language; Lytton, British Columbia is ''Camchin'' in the Thompson language (often used in English however, as Kumsheen). Canada The name ''Canada'' comes from the word meaning "village" or "settlement" in the Saint-Lawrence Iroquoian language spoken by the inhabitants of Stadacona and the neighbouring region near present-day Quebec City in the 16th century. Another contemporary meaning was "land." Jacques Cartier was first to use the word "Canada" to refer not only to the ...
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Rivers Of The Omineca Mountains
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, " burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, spr ...
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