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Classy Creek
Classy Creek is a tributary of the Tuya River in northwest part of the province of British Columbia, Canada. It flows generally southeast and south roughly Length measured using Google Maps path tool, BCGNIS coordinates, topographic maps, anToporama/ref> to join the Tuya River about north of the Tuya River's confluence with the Stikine River in the Grand Canyon of the Stikine, near Telegraph Creek Road, unofficially called Highway 51, a spur of the Stewart–Cassiar Highway. Classy Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Classy Creek is located about northeast of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about southeast of Whitehorse, Yukon. Classy Creek's watershed's land cover is classified as 46.8% shrubland, 23.3% mixed forest, 20.3% conifer forest, and small amounts of other cover. Classy Creek is in the traditional territory of the Tahltan people. Geography Classy Creek originates among unname ... [...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] |
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] |
Level Mountain Range
The Level Mountain Range is a small but prominent mountain range occupying the broad summit of Level Mountain in northern British Columbia, Canada. Located between the Tuya River in the east and the Sheslay River in the west, it represents a high point on the Nahlin Plateau. The range is geologically younger than the main mass of Level Mountain, having formed in the last 7.1 million years. An eroded stratovolcano and several lava domes of Miocene-to-Pleistocene age comprise the Level Mountain Range. The highest point is Meszah Peak Meszah Peak is a volcanic cone located north of Telegraph Creek and southwest of Zus Mountain in British Columbia, Canada. It is the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of the massive Level Mountain ... at the north end of the range with an elevation of . See also * List of volcanoes in Canada References * * Level Mountain Mountain ranges of British Columbia Stratovolcanoes of Canada Mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meszah Peak
Meszah Peak is a volcanic cone located north of Telegraph Creek and southwest of Zus Mountain in British Columbia, Canada. It is the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of the massive Level Mountain shield volcano, which forms the most voluminous and most persistent eruptive centre in the Northern Cordilleran Volcanic Province. See also * List of volcanoes in Canada * List of Northern Cordilleran volcanoes * Volcanology of Western Canada * Geography of British Columbia * Geology of the Pacific Northwest The geology of the Pacific Northwest includes the composition (including rock, minerals, and soils), structure, physical properties and the processes that shape the Pacific Northwest region of North America. The region is part of the Ring of F ... * Heart Peaks * Atsutla Range References * Catalogue of Canadian volcanoes: Meszah Peak External links * Meszah Peakin the Canadian Mountain Encyclopedia Volcanoes of British ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mansfield Creek
Mansfield Creek is a tributary of the Little Tuya River, which in turn is a tributary of the Tuya River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally south and east for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join the Little Tuya River about west-northwest of the Little Tuya's confluence with the Tuya River. Mansfield Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Mansfield Creek is located about northeast of Telegraph Creek, British Columbia, about west-southwest of Dease Lake, British Columbia, and about east of Juneau, Alaska. Mansfield Creek's watershed's land cover is classified as 40.5% shrubland, 35.3% conifer forest, 17.6% mixed forest, and small amounts of other cover. Mansfield Creek is in the traditional territory of the Tahltan First Nation, of the Tahltan people. Geography Mansfield Creek originates o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riley Creek (Middle Creek Tributary)
Riley Creek is a tributary of Middle Creek, which in turn is a tributary of the Tahltan River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally south for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join Middle Creek about north of Middle Creek's confluence with the Tahltan River. Riley Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Riley Creek is located about north of Telegraph Creek, British Columbia, about southwest of Dease Lake, British Columbia, and about east of Juneau, Alaska. Riley Creek's watershed's land cover is classified as 39.9% shrubland, 36.8% conifer forest, 20.3% mixed forest, and small amounts of other cover. Riley Creek is in the traditional territory of the Tahltan First Nation, of the Tahltan people. Geography Riley Creek originates on the southeast edge of the massive Level Mountain shield volcano, ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hartz Creek
Hartz Creek is a tributary of the Tahltan River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally south and southwest for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join the Tahltan River about north of Tahltan, British Columbia at the Tahltan River's confluence with the Stikine River. Hartz Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Hartz Creek is located about northeast of Telegraph Creek, British Columbia, about southwest of Dease Lake, British Columbia, and about east of Juneau, Alaska. Hartz Creek's watershed's land cover is classified as 44.2% shrubland, 30.7% mixed forest, 20.8% conifer forest, and small amounts of other cover. Hartz Creek is in the traditional territory of the Tahltan First Nation, of the Tahltan people. Geography Hartz Creek originates on the southeast edge of the massive Level Mountain shield ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shield Volcano
A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava erupted from a stratovolcano. Repeated eruptions result in the steady accumulation of broad sheets of lava, building up the shield volcano's distinctive form. Shield volcanoes are found wherever fluid low-silica lava reaches the surface of a rocky planet. However, they are most characteristic of ocean island volcanism associated with hot spots or with continental rift volcanism. They include the largest volcanoes on earth, such as Tamu Massif and Mauna Loa. Giant shield volcanoes are found on other planets of the Solar System, including Olympus Mons on Mars and Sapas Mons on Venus. Etymology The term 'shield volcano' is taken from the German term ''Schildvulkan'', coined by the Austrian geologist Eduard Suess in 1888 an ... [...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] |
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] |
Mixed Coniferous Forest
Mixed coniferous forest is a vegetation type dominated by a mixture of broadleaf trees and conifers.Sierra Nevada Wildflowers, Karen Wiese, 2nd ed, 2013, p 13–14 It is generally located in mountains, below the upper montane vegetation type. Sierra Nevada range In the Sierra Nevada mountain range of the western United States, the mixed coniferous forest is found at elevations of in the north, in central areas, and in the south. Characteristic conifers include Ponderosa Pine ('' Pinus ponderosa''), Sugar Pine (''Pinus lambertiana''), Incense Cedar (''Calocedrus decurrens''), White Fir (''Abies concolor''), Douglas Fir (''Pseudotsuga menziesii''), and Giant Sequoias (''Sequoiadendron giganteum'') in pockets. Characteristic broadleaved trees include Black Oak (''Quercus kelloggii''), and understory trees and shrubs, including Canyon Live Oak (''Quercus chrysolepis''), Dogwood ( ''Cornus'' spp.), Mountain Misery (''Chamaebatia foliolosa''), and Manzanitas ( ''Arctostaphylos'' spp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shrubland
Shrubland, scrubland, scrub, brush, or bush is a plant community characterized by vegetation dominated by shrubs, often also including grasses, herbs, and geophytes. Shrubland may either occur naturally or be the result of human activity. It may be the mature vegetation type in a particular region and remain stable over time, or a transitional community that occurs temporarily as the result of a disturbance, such as fire. A stable state may be maintained by regular natural disturbance such as fire or browsing. Shrubland may be unsuitable for human habitation because of the danger of fire. The term was coined in 1903. Shrubland species generally show a wide range of adaptations to fire, such as heavy seed production, lignotubers, and fire-induced germination. Botanical structural form In botany and ecology a shrub is defined as a much-branched woody plant less than 8 m high and usually with many stems. Tall shrubs are mostly 2–8 m high, small shrubs 1–2 m high and su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
