Hoodoo River
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Hoodoo River
The Hoodoo River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, located west of Hoodoo Mountain and the Twin River in Cassiar Land District. From its source in Hoodoo Glacier the Hoodoo River flows south for about Length measured using BCGNIS coordinates, topographic maps, anToporama/ref> to the Iskut River northwest of the mouth of the Craig River. The Hoodoo River's watershed covers , and its mean annual discharge is an estimated . The river's watershed's land cover is classified as 49.4% snow/glacier, 22.7% barren, 10.6% conifer forest, 9.8% shrubland, and small amounts of other cover. The mouth of the Hoodoo River is located about east-northeast of Wrangell, Alaska, about northwest of Stewart, British Columbia, and about south of Telegraph Creek, British Columbia. The Hoodoo River is in the traditional territory of the Tlingit, specifically the Shtax'héen Ḵwáan, commonly known as the Stikine River people. I ...
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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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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 ...
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Valley Glacier
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ...
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Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ..., in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as pro ...
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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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Iskut First Nation
The Iskut First Nation is a band government of the Tahltan people. Their main reserve is Iskut IR No.6, located at Iskut, British Columbia; Iskut is in the same vicinity, while the band's third reserve, Stikine River IR No. 7 is located one mile west of, and on the opposite side of the Stikine River from, the community of Telegraph Creek. The Iskut First Nation is one of two member bands of the Tahltan Nation, the other member band being the Tahltan First Nation, also known as the Tahltan Indian Band. Indian Reserves Indian Reserves under the band's administration are: * Iskut IR No.6 * Kluachon IR No.1 * Stikine River IR No.7 See also *Tahltan First Nation *Sacred Headwaters The Sacred Headwaters is a large subalpine drainage basin centred around Klappan Mountain of the Klappan Range in northern British Columbia. It is the source of three wild salmon rivers: the Skeena River, Nass River, and Stikine River. It is als ... References {{BritishColumbia-stub First Nations g ...
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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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Stikine People
The Stikine people (''Shtaxʼhéen Ḵwáan'') are a ''ḵwáan'' or regional group of the Tlingit, today based at Wrangell, Alaska. Their historical territory included Wrangell Island and other islands of the Alexander Archipelago, as well as the basin of the lower Stikine River. References See also *Taku River Tlingit *Chief Shakes Chief Shakes is a distinguished Tlingit leadership title passed down through generations among groups of native people from Northwestern North America. Lineages of the Shakes Origin The orphan Gush X’een (translation: Dorsal Fin Screen, Englis ... {{NorthAm-native-stub Tlingit ...
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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

Telegraph Creek, British Columbia
Telegraph Creek is a small community located off British Columbia Highway 37, 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 Nat ...
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Stewart, British Columbia
Stewart is a district municipality at the head of the Portland Canal in northwestern British Columbia, Canada, near the Alaskan panhandle. In 2011, its population was about 494. History The Nisga'a, who live around the Nass River, called the head of Portland Canal , meaning "safe house" or "strong house", probably because it served them as a retreat from the harassment of the Haida and Tlingit from the outer coast. They travelled in the area seasonally to pick berries and hunt birds. It and the rest of the Portland Canal had previously been the domain of the Tsetsaut people, also called the Skam-a-Kounst Indians, or in Nisga'a, an Athapaskan people who became decimated by war and disease and were driven out of the Stewart area by either Haida or Nisga'a in 1856–57. The Portland Canal was first explored and named in July 1793 by Captain George Vancouver in honour of William Cavendish-Bentinck, 3rd Duke of Portland (1738–1808), Home Secretary from 1794 to 1801. Vancouver me ...
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Wrangell, Alaska
The City and Borough of Wrangell ( tli, Ḵaachx̱ana.áakʼw, russian: Врангель) is a borough in Alaska, United States. As of the 2020 census the population was 2,127, down from 2,369 in 2010. Incorporated as a Unified Home Rule Borough on May 30, 2008, Wrangell was previously a city in the Wrangell-Petersburg Census Area (afterwards renamed the Petersburg Census Area (the Petersburg Borough was formed from part of this census area)). Its Tlingit name is ("Ḵaachx̱ans Little Lake" with ''áa-kʼw'' 'lake-diminutive'). The Tlingit people living in the Wrangell area, who were there centuries before Europeans, call themselves the after the nearby Stikine River. Alternately they use the autonym , where the meaning of is unknown. The central (urban) part of Wrangell is located at , in the northwest corner of Wrangell Island, whereas the borough now encompasses the entire eastern half of the former Wrangell-Petersburg Census Area, in addition to the area around M ...
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