Middle Creek (Tahltan River Tributary)
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Middle Creek (Tahltan River Tributary)
Middle 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 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. Middle Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Middle Creek is located about north of Telegraph Creek, British Columbia, about southwest of Dease Lake, British Columbia, and about east of Juneau, Alaska. Middle Creek's watershed's land cover is classified as 45.2% shrubland, 30.8% conifer forest, 21.4% mixed forest, and small amounts of other cover. Middle Creek is in the traditional territory of the Tahltan First Nation, of the Tahltan people. Geography Middle Creek originates on the southeast edge of the massive Level Mountain shield volcan ...
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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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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 ...
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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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Little Tuya River
The Little Tuya River is a tributary of the Tuya River in northwest part of the province of British Columbia, Canada. It flows generally south and east about Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join the Tuya River near Cariboo Meadows. The Little Tuya River's watershed covers , and its mean annual discharge is an estimated . The mouth of the Little Tuya River is located about northeast of Telegraph Creek, British Columbia, about west-southwest of Dease Lake, British Columbia, and about east of Juneau, Alaska. The river's watershed's land cover is classified as 37.8% shrubland, 28.8% conifer forest, 14.6% mixed forest, 9.2% barren, and small amounts of other cover. The Little Tuya River was named in association with the Tuya RIver. A tuya is a geologic term for a flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. The geologic term comes from Tuya Butte, which was named in association with Tuy ...
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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 ...
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Beatty Creek (Tahltan River Tributary)
Beatty Creek is a tributary of the Tahltan River in northwest part of the province of British Columbia, Canada. It flows generally south about Length measured using Google Maps path tool, BCGNIS coordinates, topographic maps, anTopoQuest/ref> to join the Tahltan River a few kilometres downstream from the Little Tahltan River confluence. The Tahltan River is one of the main tributaries of the Stikine River. Beatty Creek's watershed covers , and its mean annual discharge is . The mouth of the Beatty Creek is located about north of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about southeast of Whitehorse, Yukon. Beatty Creek's watershed's land cover is classified as 32.3% shrubland, 22.4% conifer forest, 17.8% barren, 15.8% mixed forest, 10.3% herbaceous, and small amounts of other cover. Beatty Creek is in the traditional territory of the Tahltan people. Geography Beatty Creek originates on the slopes of Meszah Peak, the highest peak of the Lev ...
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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 ...
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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 ...
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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 ...
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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-ya ...
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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 conflue ...
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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 ...
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