|
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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conifer
Conifers are a group of conifer cone, cone-bearing Spermatophyte, seed plants, a subset of gymnosperms. Scientifically, they make up the phylum, division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single extant class (biology), class, Pinopsida. All Neontology, extant conifers are perennial plant, perennial woody plants with secondary growth. The great majority are trees, though a few are shrubs. Examples include Cedrus, cedars, Pseudotsuga, Douglas-firs, Cupressaceae, cypresses, firs, junipers, Agathis, kauri, larches, pines, Tsuga, hemlocks, Sequoioideae, redwoods, spruces, and Taxaceae, 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 ecology, ecologically important. They are the dominant plants over large areas of land, most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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-ya ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 conflue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 and the second- 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 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 and the surrounding Greater Juneau Borough to form the current municipality, which is larger by area than both Rhode Island and Delaware. Downtown Juneau () is nestled at the base of Mount Juneau and across the channel from Douglas Island. As of the 2020 census, the City and Borough had a population of 32,255, making it the third-most populous city in Alaska after Anchorage and Fairbanks. Juneau experiences a daily influx o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Gi ... 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Isk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, 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 lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow
Snow comprises individual ice crystals that grow while suspended in the atmosphere—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 sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
