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Shaman Creek
Shaman Creek is a tributary of Kakiddi Lake, the source of Kakiddi Creek, and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. From its source in the glaciers south of Mount Edziza it flows generally east for roughly Lengths and distances measured using BCGNIS coordinates, topographic maps, online map servers, anToporama/ref> to empty into Kakiddi Lake, an expansion of Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River. Shaman Creek's mean annual discharge is estimated at . Its watershed covers and is mostly within Mount Edziza Provincial Park. The watershed's land cover is classified as 44.9% conifer forest, 20.7% shrubland, 16.8% barren, 10.8% herbaceous, 3.1% snow/glacier, 2.3% wetland, and small amounts of other cover. The mouth of Shaman Creek is located about southeast of Telegraph Creek, British Columbia, about north of Bob Quinn Lake, British Columbia, and about east 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 and ...
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Conifer
Conifers are a group of cone-bearing seed plants, a subset of gymnosperms. Scientifically, they make up the division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single extant class, Pinopsida. All extant conifers are perennial woody plants with secondary growth. The great majority are trees, though a few are shrubs. Examples include cedars, Douglas-firs, cypresses, firs, junipers, kauri, larches, pines, hemlocks, redwoods, spruces, and yews.Campbell, Reece, "Phylum Coniferophyta". Biology. 7th. 2005. Print. P. 595 As of 1998, the division Pinophyta was estimated to contain eight families, 68 genera, and 629 living species. Although the total number of species is relatively small, conifers are ecologically important. They are the dominant plants over large areas of land, most notably the taiga of the Northern Hemisphere, but also in similar cool climates in mountains further south. Boreal conifers have many wintertime ada ...
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Tencho Glacier
Tencho Glacier is a mountain glacier in northwestern British Columbia, Canada. It is located inside Mount Edziza Provincial Park on the Tahltan Highland, an upland area of the Stikine Plateau. Tencho Glacier is the source of several small streams that flow from the Mount Edziza volcanic complex. Etymology The name of the glacier was suggested by the Geological Survey of Canada on November 15, 1979, and eventually became official on November 24, 1980. ''Tencho'' is derived from the Tahltan words ''ten'' and ''cho'', which mean ''ice'' and ''big'' or ''great'' respectively. This glacier is so-named because it is the largest glacier of the Mount Edziza volcanic complex. Geography Tencho Glacier originates from Ice Peak and Tennena Cone on the southern flank of Mount Edziza. Its southern terminus is surrounded by Kaia Bluff in the southeast, Coffee Crater in the south and Cocoa Crater in the southwest. Unnamed tributaries of Taweh Creek originate from the southwestern side of Tencho G ...
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Cartoona Peak
Cartoona Peak is a volcanic peak at the westernmost end of Cartoona Ridge in northern British Columbia, Canada, located just southeast of Coffee Crater in Mount Edziza Provincial Park. See also *List of volcanoes in Canada * List of Northern Cordilleran volcanoes * Mount Edziza volcanic complex * Volcanism of Canada *Volcanism of Western Canada Volcanism of Western Canada has produced lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, greenstone belts, submarine volcanoes, calderas, diatremes and maars, along with examples of more less common volcanic ... References Volcanoes of the Mount Edziza volcanic complex Two-thousanders of British Columbia Lava domes Miocene volcanoes Cassiar Land District Big Raven Plateau {{BritishColumbiaInterior-geo-stub ...
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Tahltan
The Tahltan or Nahani are a First Nations people of the Athabaskan-speaking ethnolinguistic group who live in northern British Columbia around Telegraph Creek, Dease Lake, and Iskut. The Tahltan constitute the fourth division of the ''Nahane'' (People of the West). Culture The Tahltan cultural practices and lifeways varied widely as they were often widely separated and would have to endure varying conditions depending on their locality. In Tahltan culture it was believed that some of their ancestors had knowledge that others did not from times before a great flood. Some of these ancestors used that knowledge for the good of the people, while others used it for evil and to the disadvantage of others. Raven is considered to be the protagonist hero against these evil ancestors. Social organization Tahltan social organization is founded on matriarchy and intermarriage between two main clan designations. The two main clans of Tahltan people are Tses' Kiya (pronounced Tses-kee-y ...
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Tahltan First Nation
The Tahltan First Nation, also known as the Tahltan Indian Band, is a band government of the Tahltan people. Their main community and reserves are located at Telegraph Creek, British Columbia. Their language is the Tahltan language, which is an Athabaskan language also known as Nahanni, is closely related to Kaska and Dunneza. Their Indian and Northern Affairs Canada band number is 682. The Tahltan First Nation is joined with the Iskut First Nation in a combined tribal council-type organization known as the Tahltan Nation. Population Registered band population is 1,668. Indian Reserves Indian Reserves under the administration of the Tahltan First Nation are: * Classy Creek IR No.8, 1 mile south of Mincho Lake, 5 miles north of the confluence of Classy Creek and the Tuya River, 259 ha. * Dease Lake IR No.9, near south end of Dease Lake, opposite the settlement of Dease Lake, 129.50 ha. * Guhthe Tah IR No.12, 30.40 ha. * Hiusta's Meadow IR No.2, 3 miles north of the con ...
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Juneau, Alaska
The City and Borough of Juneau, more commonly known simply as Juneau ( ; tli, Dzánti K'ihéeni ), is the capital city of the state of Alaska. Located in the Gastineau Channel and the Alaskan panhandle, it is a unified municipality A municipality is usually a single administrative division having municipal corporation, corporate status and powers of self-government or jurisdiction as granted by national and regional laws to which it is subordinate. The term ''municipality ... and the second-List of United States cities by area, largest city in the United States by area. Juneau was named the capital of Alaska in 1906, when the government of what was then the District of Alaska was moved from Sitka, Alaska, Sitka as dictated by the U.S. Congress in 1900. The municipality unified on July 1, 1970, when the city of Juneau merged with the city of Douglas, Alaska, Douglas and the surrounding Greater Juneau Borough (United States), Borough to form the current municipality, which ...
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Bob Quinn Lake
Bob Quinn Lake is an unincorporated community in northwestern British Columbia, Canada. It is located along the Stewart-Cassiar Highway (Highway 37) along Bob Quinn Lake, about north of Kitwanga Kitwanga or Gitwangak or Gitwangax ("people of the place of rabbits" in the Gitxsan language) is located where the Kitwanga River runs into the Skeena River in British Columbia. A long-standing village before contact, the village is within ... and south of Dease Lake. Both the locality and the lake are named after Robert Quinn, an area old timer and one-time lineman on the Yukon Telegraph Line. References Unincorporated settlements in British Columbia Populated places in the Regional District of Kitimat–Stikine Stikine Country {{KitimatStikine-geo-stub ...
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Telegraph Creek
Telegraph Creek is a small community located off 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 Nation of the settlement of ...
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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 saltwater. The main wetland typ ...
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Glacier
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 ...
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Snow
Snow comprises individual ice crystals that grow while suspended in the atmosphere An atmosphere () is a layer of gas or layers of gases that envelop a planet, and is held in place by the gravity of the planetary body. A planet retains an atmosphere when the gravity is great and the temperature of the atmosphere is low. ...—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or Sublimation (phase transition), sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes Nucleation, nucleate around particles in the atmosphere by attracting supercooling, supercooled water droplets, which ...
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