|
Shuswap Lake
Shuswap Lake (pronounced /ˈʃuːʃwɑːp/) is a lake located in the southern interior of British Columbia, Canada that drains via the Little Shuswap River into Little Shuswap Lake. Little Shuswap Lake is the source of the South Thompson River, a branch of the Thompson River, a tributary of the Fraser River. It is at the heart of a region known as the Columbia Shuswap or "the Shuswap", noted for its recreational lakeshore communities including the city of Salmon Arm. The name "Shuswap" is derived from the Shuswap or Secwepemc First Nations people, the most northern of the Interior Salish peoples, whose territory includes the Shuswap. The Shuswap call themselves /ʃǝxwépmǝx/ in their own language, which is called /ʃǝxwepmǝxtʃín/. Geography The central interior plateau of British Columbia drained by the Fraser and Okanagan rivers is part of the Shuswap terrane in British Columbia and northern Washington state. It is dissected by numerous elongated, glacially- overdeep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chinook Salmon
The Chinook salmon (''Oncorhynchus tshawytscha'') is the largest and most valuable species of Pacific salmon in North America, as well as the largest in the genus ''Oncorhynchus''. Its common name is derived from the Chinookan peoples. Other vernacular names for the species include king salmon, Quinnat salmon, Tsumen, spring salmon, chrome hog, Blackmouth, and Tyee salmon. The scientific species name is based on the Russian common name ''chavycha'' (чавыча). Chinook are anadromous fish native to the North Pacific Ocean and the river systems of western North America, ranging from California to Alaska, as well as Asian rivers ranging from northern Japan to the Palyavaam River in the Arctic northeast Siberia. They have been introduced to other parts of the world, including New Zealand, thriving in Lake Michigan Great Lakes of North America and Michigan's western rivers, and Patagonia. A large Chinook is a prized and sought-after catch for a sporting angler. The flesh of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sicamous
Sicamous is a district municipality in British Columbia located adjacent to the Trans-Canada Highway at the Highway 97A junction, where Mara Lake empties into Shuswap Lake via a short narrows. Sicamous is a resort town about halfway between Calgary and Vancouver and is the eastern gateway to the Apple Country. With of shoreline, it styles itself as the houseboat capital of Canada. It has a population of 2,613 according to a 2021 census. Name origin Sicamous is an adaptation of a Shuswap language word meaning "river circling mountains". History In the 1800s, Sicamous and area was inhabited by a semi-nomadic Indigenous nation called the Secwepemc or Shuswap. They crossed the Rocky Mountains to hunt buffalo on the plains. In this area they were called the "Schickamoos". In 1872, a Provincial Map shows Schickamoos Narrows, which in early history was known as a "meeting place of Indians". In 1864, gold was discovered on the Columbia River. Seymour Arm became a supply centre in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monashees
The Monashee Mountains are a mountain range lying mostly in British Columbia, Canada, extending into the U.S. state of Washington. They stretch from north to south and from east to west. They are a sub-range of the Columbia Mountains. The highest summit is Mount Monashee, which reaches . The name is from the Scottish Gaelic ''monadh'' and ''sìth,'' meaning "moor" and "peace". Geography The Monashee Mountains are limited on the east by the Columbia River and Arrow Lakes, beyond which lie the Selkirk Mountains. They are limited on the west by the upper North Thompson River and the Interior Plateau. The northern end of the range is Canoe Mountain at the south end of the Robson Valley, near of the town of Valemount, British Columbia. The southern extremity of the range is in Washington State, where the Kettle River Range reaches the confluence of the Kettle River and the Columbia, and reaches west to the southern extremity of the Okanagan Highland (spelled Okanogan Highland in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eagle Pass (British Columbia)
Eagle Pass (elevation ) is a mountain pass through the Gold Range of the Monashee Mountains in British Columbia, Canada. It divides the Columbia River drainage basin from that of the Fraser River (via the Shuswap Lakes and the Thompson River). Eagle Pass was chosen as the route of the Canadian Pacific Railway (CPR), and later the Trans-Canada Highway, over the Monashees. The line over the Eagle Pass was the last section of the CPR to be completed; the last spike was driven at a location known as Craigellachie in 1885. The pass was discovered by Walter Moberly in his role as Assistant Surveyor General of British Columbia in 1865. The nearest city to Eagle Pass is Revelstoke, 20 kilometres to the east. See also *Eagle River (Shuswap) The Eagle River is a river in the Canadian province of British Columbia. The river was named by Walter Moberly after following the flight of eagles and finding Eagle Pass. Course The Eagle River originates in the mountains west of Revelstok ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salmon Arm
Salmon Arm is a city in the Columbia Shuswap Regional District of the Southern Interior of the Canadian province of British Columbia that has a population of 17,706 (2016). Salmon Arm was incorporated as a municipal district on May 15, 1905. The city of Salmon Arm separated from the district in 1912, but was downgraded to a village in 1958. In 1970, the city of Salmon Arm once again reunited with the District Municipality. Salmon Arm once again became a city in 2005, and is now the location of the head offices of the Columbia-Shuswap Regional District. It is a tourist town in the summer, with many beaches, camping facilities and house boat rentals. Salmon Arm is home to the longest wooden freshwater wharf in North America. Etymology Salmon Arm takes its name from its place along Shuswap Lake. The lake has four "arms": Shuswap Arm in the west, Seymour Arm in the north, Anstey Arm in the northeast, and Salmon Arm in the south, named after the large runs of salmon that used to run ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salmon River (Shuswap Lake)
The Salmon River is a river in the Shuswap region of British Columbia, Canada. The river arises in the mountains between Kamloops and Kelowna. It flows west to Salmon Lake, then issues northeastward and descends into a broad valley near Westwold. It then runs east along the route of Highway 97 past the town of Falkland before turning north again through the Silver Creek area to flow into the Salmon Arm of Shuswap Lake at Salmon Arm. For several kilometres upstream and downstream of Westwold the river runs through a deep gravel bed; in this section it has no surface flow except during freshet in any year that is not exceptionally wet. This presents a barrier to migratory fish. The river takes its name from the numerous salmon that spawned in the river prior to 1914, the year of the Hell's Gate Slide. Since then the salmon run ''Salmon Run'' is a 1982 video game for the Atari 8-bit family created by Bill Williams and distributed via the Atari Program Exchange. ''Salmon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adams Lake
Adams Lake is a large, deep, coldwater lake in British Columbia, Canada; its average depth ranks 6th in the world. The southern end of the lake is approximately north of the town of Chase in the Shuswap Country region of British Columbia. The lake's upper reaches lie in the northern Monashee Mountains, while its lower end penetrates the Shuswap Highland. The lake supports Chinook, Sockeye and Coho salmon, Kokanee, mountain whitefish and rainbow trout. Geography The lake is long and between and wide. The surface elevation is above sea level. The lake is very deep; with a mean depth of and maximum depth of it is the second deepest lake in British Columbia (next to Quesnel Lake, which has a maximum depth of ) and 6th deepest lake in the world by mean depth. Water flows into the lake though many tributaries (most notably the Upper Adams River, , and Bush Creek). The water drains from the lake as the Lower Adams River which is home to a very large and famous sockeye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arm (geography)
In geography, an arm is a narrow extension, inlet, or smaller reach, of water flowing out from a much larger body of water, such as an ocean, a sea, or a lake. Although different geographically, a sound or bay may also be called an arm. Both the tributary and distributary of a river are sometimes called an "arm". By extension, a ''canal arm'' is a subsidiary branch of a canal or inland waterway. See also *River *Channel *Indian Arm *Alice Arm *Gulf of Bothnia The Gulf of Bothnia (; fi, Pohjanlahti; sv, Bottniska viken) is divided into the Bothnian Bay and Bothnian Sea, and it is the northernmost arm of the Baltic Sea, between Finland's west coast ( East Bothnia) and the Sweden's east coast (West ... Coastal and oceanic landforms Bodies of water {{Topography-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Overdeepening
Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are hundreds of metres below the deepest continuous line (the thalweg) along a valley or watercourse. This phenomenon is observed under modern day glaciers, in salt-water fjords and fresh-water lakes remaining after glaciers melt, as well as in tunnel valleys which are partially or totally filled with sediment. When the channel produced by a glacier is filled with debris, the subsurface geomorphic structure is found to be erosionally cut into bedrock and subsequently filled by sediments. These overdeepened cuts into bedrock structures can reach a depth of several hundred metres below the valley floor. Overdeepened fjords and lakes have significant economic value as harbours and fisheries. Overdeepened basins and valleys filled with sediment (termed tunnel valleys) are of particular interest to engineers, petroleum geologists, and hydrologists; ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Fjord")
