Teslin Plateau
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Teslin Plateau
The Teslin Plateau is a sub-plateau, of the Yukon Plateau physiographic section, in northern British Columbia, Canada, located north of the Nakina River between Atlin Lake and Teslin Lake. See also *Atlin Volcanic Field *Nisutlin Plateau The Nisutlin Plateau is a sub-plateau, of the Yukon Plateau physiographic section, in northern British Columbia, Canada, extending east from Teslin Lake Teslin Lake is a large lake spanning the border between British Columbia and Yukon, Canada. ... References Plateaus of British Columbia Atlin District {{BritishColumbiaInterior-geo-stub ...
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Teslin Lake
Teslin Lake is a large lake spanning the border between British Columbia and Yukon, Canada. It is one of a group of large lakes in the region of far northwestern BC, east of the upper Alaska Panhandle, which are the southern extremity of the basin of the Yukon River, and which are known in Yukon as "the Southern Lakes" (the other major ones in the group are Atlin Lake and Tagish Lake but include Bennett and Lindeman Lakes, the headwaters of the Yukon River itself). The lake is fed and drained primarily by the Teslin River, south and north, but is also fed from the east by the Jennings River and the Swift River, and from the west by the Hayes River. According to the Yukon Geographical Names Project, "Teslin" means "long water", but in the Tlingit language the local ''kwaan'' or tribe of Tlingit is called ''Deisleen Kwáan"'', meaning "Big Sinew Tribe". There are three Taku River Tlingit First Nation communities around the south end of the lake in British Columbia: Jenni ...
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British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ...
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Yukon
Yukon (; ; formerly called Yukon Territory and also referred to as the Yukon) is the smallest and westernmost of Canada's three territories. It also is the second-least populated province or territory in Canada, with a population of 43,964 as of March 2022. Whitehorse, the territorial capital, is the largest settlement in any of the three territories. Yukon was split from the North-West Territories in 1898 as the Yukon Territory. The federal government's ''Yukon Act'', which received royal assent on March 27, 2002, established Yukon as the territory's official name, though ''Yukon Territory'' is also still popular in usage and Canada Post continues to use the territory's internationally approved postal abbreviation of ''YT''. In 2021, territorial government policy was changed so that “''The'' Yukon” would be recommended for use in official territorial government materials. Though officially bilingual (English and French), the Yukon government also recognizes First Nati ...
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Yukon Plateau
The Yukon Plateau is a plateau (also defined as a plain) located in the Yukon Territory, comprising much of the central and southern Yukon Territory and the far northern part of British Columbia, Canada between Tagish Lake (W) and the Cassiar Mountains (E) and north of the Nakina River. Sub-plateaus include the Teslin Plateau and the Nisutlin Plateau, west and east of Teslin Lake, respectively. See also * Yukon Interior dry forests *Yukon Ranges The Yukon Ranges are a mountain range comprising the mountains in the southeastern part of the U.S. state of Alaska and most of the Yukon in Canada. Named after the Yukon, this range has area of .Plateaus of Canada ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of ...
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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 an ...
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Nakina River
The Nakina River is a river in northwestern British Columbia, Canada, rising southeast of Atlin Lake and flowing generally southeast to its confluence with the Inklin River at the locality of Inklin, where the two rivers combine to form the Taku River. A major tributary of the Nakina is the Sloko River, which runs Northeast to meet it from the area of the Llewellyn Glacier of the Juneau Icefield The Juneau Icefield is an ice field located just north of Juneau, Alaska, continuing north through the border with British Columbia, extending through an area of in the Coast Range ranging north to south and east to west. The icefield is the so .... References * Rivers of British Columbia Atlin District Taku Plateau {{BritishColumbiaInterior-river-stub ...
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Atlin Lake
Atlin Lake ( Lingít: ''Áa Tlein'') is the largest natural lake in the Canadian province of British Columbia. The northern tip of the lake is in Yukon, as is Little Atlin Lake. However, most of the lake lies within the Atlin District of British Columbia. Atlin Lake is generally considered to be the source of the Yukon River although it is drained via the short Atlin River into Tagish Lake. Atlin Lake was named by the Tlingit First Nation people of the region. The name comes from ''Áa Tlein'' (in Canadian spelling ''Â Tłèn''), the Tlingit name meaning simply "big lake". The community of Atlin, British Columbia, is located on the eastern shore of the lake. The southern part of the lake is in the Atlin Provincial Park and Recreation Area. See also * Atlin Mountain Atlin Mountain, at , is a medium-sized mountain located next to Atlin Lake in the northern end of the Coast Mountain range in British Columbia, Canada Canada is a country in North America. Its ...
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Atlin Volcanic Field
The Atlin Volcanic Field, also called the Llangorse Volcanic Field and the Surprise Lake Volcanic Field, is a group of late-Pleistocene to Holocene cinder cones that lies on the Teslin Plateau east of Atlin Lake, Canada. The largest volcanic feature is the 1880-m-high Ruby Mountain which has been partially dissected by Pleistocene and post-Wisconsin glaciation. Two basaltic cinder cones at the heads of Cracker Creek and Volcanic Creek lie within glacially dissected U-shaped valleys and may be of postglacial age. November 8, 1898, eruption A Yukon newspaper reported in 1898 that an eruption was occurring near Atlin about 80 km south of Gladys Lake. Miners working in the area reportedly were able to work during the dark nights, due to the glow of the eruption. The article also reported that a group of people were going down from the Yukon to investigate the eruption, but no further reports were apparently made. Several recent studies, including a summary by Edwards et al ...
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Nisutlin Plateau
The Nisutlin Plateau is a sub-plateau, of the Yukon Plateau physiographic section, in northern British Columbia, Canada, extending east from Teslin Lake Teslin Lake is a large lake spanning the border between British Columbia and Yukon, Canada. It is one of a group of large lakes in the region of far northwestern BC, east of the upper Alaska Panhandle, which are the southern extremity of the bas ... to the Cassiar Mountains. See also * Teslin Plateau References *Nisutlin Plateauin the Canadian Mountain Encyclopedia Plateaus of British Columbia Stikine Ranges {{BritishColumbiaInterior-geo-stub ...
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Plateaus Of British Columbia
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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