Great Glacier
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Great Glacier
Great Glacier Provincial Park is a provincial park located in the Stikine Country region of British Columbia, Canada. It was established on January 25, 2001 to protect Great Glacier and the surrounding mountainous terrain. The park lies in the traditional territory of the Tahltan First Nation about south of the Tahltan community of Telegraph Creek. History According to the legends of the Tahltan and Tlingit First Nations, Great Glacier once spanned the entire width of the Stikine River to meet the toe of Choquette Glacier on the eastern side of the valley. The glacier was also the site of the last major battle between the Tahltan and Tlingit First Nations many generations ago. Geography Great Glacier Park is located in the Boundary Ranges of British Columbia between the lower Stikine River and the Alaska-British Columbia boundary. Immediately across the river from Great Glacier Park is Choquette Hot Springs Provincial Park, which protects a collection of hot springs and assoc ...
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Choquette Hot Springs Provincial Park
Choquette Hot Springs Provincial Park is a provincial park located in the Stikine Country region of British Columbia, Canada. It was established on January 25, 2001, to protect Stikine River Hot Springs, the largest hot springs on the Canadian side of the lower Stikine River. The park lies in the traditional territory of the Tahltan First Nation about south of the Tahltan community of Telegraph Creek. Geography The park is located on the eastern banks of the Stikine River, just north of the river's confluence with the Choquette River. Despite the park's name, the official name of the hot springs is ''Stikine River Hot Springs''. Geology The Stikine River Hot Springs are a collection of over 15 individual hot springs that emerge out from the granitic rocks at the base of the valley wall, or from mud just beyond the valley floor. Many of these hot springs are within a tidally-influenced area and are underwater at high tides. At least four hot springs remain above the high tide and ...
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Boundary Ranges
The Boundary Ranges, also known in the singular and as the Alaska Boundary Range, are the largest and most northerly subrange of the Coast Mountains. They begin at the Nass River, near the southern end of the Alaska Panhandle in the Canadian province of British Columbia and run to the Kelsall River, near the Chilkoot Pass, beyond which are the Alsek Ranges of the Saint Elias Mountains, and northwards into the Yukon Territory flanking the west side of the Yukon River drainage as far as Champagne Pass, north of which being the Yukon Ranges. To their east are the Skeena Mountains and Stikine Plateau of the Interior Mountains complex that lies northwest of the Interior Plateau; the immediately adjoining subregion of the Stikine Plateau is the Tahltan Highland. To their northeast is the Tagish Highland, which is a subregion of the Yukon Plateau. Both highlands are considered in some descriptions as included in the Coast Mountains. The Alexander Archipelago lies offshore and is ...
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Provincial Parks Of British Columbia
Provincial may refer to: Government & Administration * Provincial capitals, an administrative sub-national capital of a country * Provincial city (other) * Provincial minister (other) * Provincial Secretary, a position in Canadian government * Member of Provincial Parliament (other), a title for legislators in Ontario, Canada as well as Eastern Cape Province, South Africa. * Provincial council (other), various meanings * Sub-provincial city in the People's Republic of China Companies * The Provincial sector of British Rail, which was later renamed Regional Railways * Provincial Airlines, a Canadian airline * Provincial Insurance Company, a former insurance company in the United Kingdom Other Uses * Provincial Osorno, a football club from Chile * Provincial examinations, a school-leaving exam in British Columbia, Canada * A provincial superior of a religious order * Provincial park, the equivalent of national parks in the Canadian province ...
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Glaciers Of British Columbia
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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Stikine, British Columbia
Stikine, also known formerly as Boundary, is an unincorporated locality and former customs post on the Stikine River, located on the Canadian side of the British Columbia-Alaska boundary on the Stikine River's west (right) bank. The customs post was seasonal and operated in the summer months only. The name Boundary was in use from 1930 to 1964, with designation "Customs Post" changed in 1955 to "locality". See also *Stikine Country *Stikine Gold Rush *Stikine Region *Fort Stikine *Choquette Hot Springs Provincial Park *Great Glacier Provincial Park *Boundary Falls, British Columbia Boundary Falls is a locality in the Boundary Country The Boundary Country is a historical designation for a district in southern British Columbia lying, as its name suggests, along the boundary between Canada and the United States. It lies to th ... (also known as Boundary) References * * External linksImage of "Boundary House" on Panoramio.com Unincorporated settlements in British Columbia St ...
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Wetland
A wetland is a distinct ecosystem that is flooded or saturated by water, either permanently (for years or decades) or seasonally (for weeks or months). Flooding results in oxygen-free (anoxic) processes prevailing, especially in the soils. The primary factor that distinguishes wetlands from terrestrial land forms or Body of water, water bodies is the characteristic vegetation of aquatic plants, adapted to the unique anoxic hydric soils. Wetlands are considered among the most biologically diverse of all ecosystems, serving as home to a wide range of plant and animal species. Methods for assessing wetland functions, wetland ecological health, and general wetland condition have been developed for many regions of the world. These methods have contributed to wetland conservation partly by raising public awareness of the functions some wetlands provide. Wetlands occur naturally on every continent. The water in wetlands is either freshwater, brackish or seawater, saltwater. The main w ...
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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 circulation through faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its ...
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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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Glacier Terminus
A glacier terminus, toe, or snout, is the end of a glacier at any given point in time. Although glaciers seem motionless to the observer, in reality glaciers are in endless motion and the glacier terminus is always either advancing or retreating. The location of the terminus is often directly related to glacier mass balance, which is based on the amount of snowfall which occurs in the accumulation zone of a glacier, as compared to the amount that is melted in the ablation zone. The position of a glacier terminus is also impacted by localized or regional temperature change over time. Tracking Tracking the change in location of a glacier terminus is a method of monitoring a glacier's movement. The end of the glacier terminus is measured from a fixed position in neighboring bedrock periodically over time. The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of trac ...
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Regional District Of Kitimat-Stikine
In geography, regions, otherwise referred to as zones, lands or territories, are areas that are broadly divided by physical characteristics (physical geography), human impact characteristics (human geography), and the interaction of humanity and the environment (environmental geography). Geographic regions and sub-regions are mostly described by their imprecisely defined, and sometimes transitory boundaries, except in human geography, where jurisdiction areas such as national borders are defined in law. Apart from the global continental regions, there are also hydrospheric and atmospheric regions that cover the oceans, and discrete climates above the land and water masses of the planet. The land and water global regions are divided into subregions geographically bounded by large geological features that influence large-scale ecologies, such as plains and features. As a way of describing spatial areas, the concept of regions is important and widely used among the many branches of ...
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Telegraph Creek, British Columbia
Telegraph Creek is a small community located off British Columbia Highway 37, Highway 37 in northern British Columbia at the confluence of the Stikine River and Telegraph Creek. The only permanent settlement on the Stikine River, it is home to approximately 250 members of Tahltan First Nation and non-native residents. The town offers basic services, including Anglican and Catholic churches, a general store, a post office, a clinic with several nurses on-call around the clock, two Royal Canadian Mounted Police officers, and a K-9 school. Steep river banks and rocky gorges form the terraced nature of the geography. The community includes Telegraph Creek Indian Reserve No. 6, Telegraph Creek Indian Reserve No. 6A, and Guhthe Tah Indian Reserve No. 12 which are under the governance of the Tahltan First Nation of Telegraph Creek. Stikine Indian Reserve No. 7, which is one mile west (downstream) and on the opposite side of the Stikine River, is under the governance of the Iskut First Nat ...
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