Kaha Creek
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Kaha Creek
Kaha Creek is a tributary of the Koshin River in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly Length measured using Google Maps path tool, BCGNIS coordinates, topographic maps, anToporama/ref> to join the Koshin River about north of Hatin Lake, and about north of Callison Ranch. Kaha Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Kaha Creek is located about north of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about west of Dease Lake, British Columbia. Kaha Creek's watershed's land cover is classified as 41.1% conifer forest, 40.2% shrubland, 12.3% barren, and small amounts of other cover. Kaha Creek is in the traditional territory of the Tlingit Taku River Tlingit First Nation and the Tahltan First Nation, of the Tahltan people. Geography Kaha Creek originates on the north side of the massive Level Mountain shield volcano, near the headwaters 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 an ...
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Land Cover
Land cover is the physical material at the surface of Earth. Land covers include grass, asphalt, trees, bare ground, water, etc. Earth cover is the expression used by ecologist Frederick Edward Clements that has its closest modern equivalent being vegetation.Makers of American Botany, Harry Baker Humphrey, Ronald Press Company, Library of Congress Card Number 61-18435 The expression continues to be used by the United States Bureau of Land Management. There are two primary methods for capturing information on land cover: field survey and analysis of remotely sensed imagery. Land change models can be built from these types of data to assess changes in land cover over time. One of the major land cover issues (as with all natural resource inventories) is that every survey defines similarly named categories in different ways. For instance, there are many definitions of "forest"—sometimes within the same organisation—that may or may not incorporate a number of different forest fe ...
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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 at the north end of the range with an elevation of . See also *List of volcanoes in Canada List of volcanoes in Canada is an incomplete list of volcanoes found in Mainland Canada, in the Canadian islands and in Canadian waters. All but one province, Prince Edward Island, have at least one volcano. Alberta British Columbia Ne ... References * * Level Mountain Mountain ranges of British Columbia Stratovolcanoes of Canada ...
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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 * Heart Peaks * Atsutla Range The Atsutla Range is a granitic mountain range on the Kawdy Plateau in northern British Columbia, Canada. The Atsutla Range lies south of the Yukon border in between Teslin Lake and the Stewart-Cassiar Highway, roughly north-northeast of Dease L ... References * Catalogue of Canadian volcanoes: Meszah Peak External links * Meszah Peakin the Canadian Mountain Encyclopedia Volcanoes of Briti ...
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Megatushon Creek
Megatushon Creek is a tributary of the Nahlin River, part of the Taku River watershed in northwest part of the province of British Columbia, Canada. It flows generally northeast and east for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join the Nahlin River not far from the Nahlin's source south of Tachilta Lakes. Megatushon Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Megatushon Creek is located about west of Dease Lake, British Columbia, about north of Telegraph Creek, British Columbia, and about east of Juneau, Alaska. Megatushon Creek's watershed's land cover is classified as 34.8% barren, 32.3% shrubland, 24.8% conifer forest, and small amounts of other cover. Megatushon Creek is in the traditional territory of the Tlingit Taku River Tlingit First Nation and the Tahltan First Nation, of the Tahltan people. Geography Megatushon Creek originates on the east side of the massive Lev ...
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Matsatu Creek
Matsatu Creek, historically called the Matsatu River, is a tributary of Kakuchuya Creek and part of the Taku River watershed in northwest part of the province of British Columbia, Canada. It is located north of the abandoned settlement of Sheslay in Cassiar Land District. From its source at Level Mountain, where it has cut a large gorge into its western escarpment, Matsatu Creek flows generally north and west for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join Kakuchuya Creek, the main tributary of the Dudidontu River. The Dudidontu River in turn flows into the Nahlin River, a tributary of the Inklin River, which flows into the Taku River. Matsatu Creek's mean annual discharge is estimated at . Its watershed covers . The watershed's land cover is classified as 52.7% barren, 28.6% shrubland, 10.1% conifer forest, 5.0% herbaceous, and small amounts of other cover. The mouth of Matsatu Creek is located about north of Telegra ...
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Lost Creek (Koshin River)
Lost Creek is a tributary of the Koshin River in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to join the Koshin River just north of Hatin Lake, and about north of Callison Ranch. Lost Creek's watershed covers , and its mean annual discharge is estimated at . The mouth of Lost Creek is located about north of Telegraph Creek, British Columbia, about west of Dease Lake, British Columbia, and about east of Juneau, Alaska. Lost Creek's watershed's land cover is classified as 46.3% shrubland, 31.5% conifer forest, 12.2% barren, and small amounts of other cover. Lost Creek is in the traditional territory of the Tlingit Taku River Tlingit First Nation and the Tahltan First Nation, of the Tahltan people. Geography Lost Creek originates on the north side of the massive Level Mountain shield volcano, near the headwaters of Kaha Creek and Matsatu C ...
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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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Taku River Tlingit First Nation
The Taku River Tlingit First Nation are the band government of the Inland Tlingit in far northern British Columbia, Canada and also in Yukon. They comprise two ''ḵwaan'' (tribes) of the Tlingit people, who are otherwise coastal, the ''Áa Tlein Ḵwáan'' of the Atlin Lake area and the ''Deisleen Ḵwáan'' of Teslin Lake, whose main focus is the Teslin Tlingit Council in Teslin, Yukon. Their band offices are in Atlin, British Columbia. Indian Reserves Despite their presence in Yukon, all Taku River Tlingit Indian Reserves are located in British Columbia:Indian and Northern Affairs Canada - Reserves/Settlements/Villages Detail
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Tlingit
The Tlingit ( or ; also spelled Tlinkit) are indigenous peoples of the Pacific Northwest Coast of North America. Their language is the Tlingit language (natively , pronounced ),"Lingít Yoo X'atángi: The Tlingit Language."
''Sealaska Heritage Institute.'' (retrieved 3 December 2009)
in which the name means 'People of the Tides'.Pritzker, 208 The Russian name ' (, from a Sugpiaq-Alutiiq term ' for the worn by women) or the related German name ' may be encountered referring to the people in older historical literature, such as