Klastline Plateau
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Klastline Plateau
The Klastline Plateau is a plateau in the Stikine Region of the Northern Interior of British Columbia, Canada. A subplateau of the Stikine Plateau, it is located between the Stikine River (N), the upper Iskut River (S), Mess Creek (W) and the Klappan River (E). The Skeena Mountains are to the south, the Tahltan Highland to the west, the Spatsizi Plateau to the east, and the Tanzilla Plateau The Tanzilla Plateau is a plateau in the Stikine Country of the Northern Interior of British Columbia, Canada. It is a sub-plateau of the Stikine Plateau and is located east of the Tuya River, north of the Stikine River and surrounding Dease Lak ... to the north, on the other side of the Stikine. The Spatsizi and Tanzilla Plateaus, and the Tahltan Highland, are also part of the Stikine Plateau. References * Plateaus of British Columbia Stikine Country Stikine Plateau Volcanism of British Columbia {{BritishColumbiaInterior-geo-stub ...
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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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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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Stikine Plateau
The Stikine Plateau is a plateau in northern British Columbia, Canada. It lies between the Boundary Ranges of the Coast Mountains on the west and southwest and the Cassiar Mountains along its northeast, and between the Skeena Mountains on its south and southeast and the Jennings and Nakina Rivers on the north. Sub-plateaus and mountain ranges The plateau has a number of sub-plateaus:''Map of the Canadian Cordillera''
ancillary document t
''Landforms of British Columbia'', S. Holland, Bulletin 48, Ministry of Energy, Mines and Resources, BC Govt, 1976
*th ...
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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 lava. The un ...
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Stikine Region
The Stikine Region is an unincorporated area in northwestern British Columbia, Canada. It is the only area in the province that is not part of a regional district. The Stikine Region was left unincorporated following legislation that established the province's regional districts in 1968 and is not classified as a regional district. It contains no municipal governments which normally constitute the majority of seats on the boards of regional districts. There is only one local planning area, the Atlin Community Planning Area, which was combined in 2009 with the Atlin Community Improvement District to provide fire, landfill, water, streetlighting, sidewalks and advisory land use services. All other services not provided privately are administered directly by various provincial government ministries. The area around Dease Lake, formerly in the Stikine Region, is now within the boundaries of the Regional District of Kitimat–Stikine following a boundary amendment in 2008. The Stik ...
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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_km2 ...
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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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Iskut River
The Iskut River, located in the northwest part of the province of British Columbia is the largest tributary of the Stikine River, entering it about above its entry into Alaska. From its source at Kluachon Lake the Iskut River flows south and west for about Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to the Stikine River near the border of British Columbia and Alaska. The upper Iskut flows south through a series of lakes: Kluachon Lake, Eddontenajon Lake, Tatogga Lake, Kinaskan Lake, Natadesleen Lake, and others. The middle Iskut encompasses the area between the Little Iskut River and Forrest Kerr Creek. Below the Ningunsaw River the Iskut flows southwest through a canyon and is regulated by the Forrest Kerr Hydroelectric Project, a run-of-river hydroelectric project. The lower Iskut flows west through an increasingly braided channel. The upper Iskut is in the Klastline Plateau, a subregion of the Stikine Plateau. The middle Iskut forms the bou ...
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Mess Creek
Mess Creek is a tributary of the Stikine River, southwest of Mount Edziza in Mount Edziza Provincial Park and Recreation Area in northern British Columbia, Canada. The creek and its tributaries have several hot spring A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circ ...s. Mess Lake, a small body of water on Mess Creek, has warm springs. Sezill Hot Springs is on Sezill Creek. References {{reflist Rivers of British Columbia ...
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Klappan River
The Klappan River is a major tributary of the Stikine River in northwestern British Columbia, Canada. It flows north from an area known as the Sacred Headwaters, which is the source not only of this river but also of the Nass, Skeena, Spatsizi and Stikine Rivers. The headwaters region is the site of a controversial coal-bed methane project. See also *Klappan Range The Klappan Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Klappan River and Iskut River in northern British Columbia, Canada. Mountains Mountains within the Klappan Range include: * Todagin Mountain ... * Klappan Mountain References *https://web.archive.org/web/20110706165819/http://archive.ilmb.gov.bc.ca/bcgn-bin/bcg10?name=5410 Stikine Country Stikine Plateau Rivers of British Columbia Tributaries of the Stikine River Cassiar Land District {{BritishColumbiaInterior-river-stub ...
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Skeena Mountains
The Skeena Mountains, also known as the Skeenas, are a subrange of the Interior Mountains of northern British Columbia, Canada, essentially flanking the upper basin of the Skeena River. They lie just inland from the southern end of the Boundary Ranges of the Coast Mountains, and also of the northern end of the Kitimat Ranges (another subrange of the Coast Mountains). Their southern limit is described by the Bulkley River (a major tributary of the Skeena; its valley and that of the lower Skeena River are used by BC Highway 16) and the upper northwestern reaches of Babine and Takla Lakes, and on their northeast by the upper reaches of the Omineca River. To the north the Skeenas abut the southern Tahltan Highland and Klastline Plateau, part of the southern reaches of the Stikine Plateau and the Spatsizi Plateau, another subplateau of the Stikine Plateau, which includes the uppermost part of the course of the Stikine River. To the northwest, across the narrow confines of the Spatsiz ...
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Tahltan Highland
The Tahltan Highland is an upland area of plateau and relatively lower mountain ranges in British Columbia, Canada, lying east of the Boundary Ranges and south of the Inklin River (the east fork of the Taku River). Its eastern boundary is formed by the Sheslay River and the Little Tuya River, while its southern boundary extends across the Stikine River and its Grand Canyon of the Stikine, Grand Canyon to include the Mount Edziza volcanic complex (which includes the Spectrum Range), and the Zagoddethchino massif. References

*S. Holland. ''Landforms of British Columbia'', BC Government Department of Energy Mines and Resources (1976). * Tahltan Highland, Stikine Country Stikine Plateau Plateaus of British Columbia {{BritishColumbiaInterior-geo-stub ...
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