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Klinaklini Canyon
Klinaklini Canyon is a canyon on the Klinaklini River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, located to the north of the head of Knight Inlet in the river's lowermost reaches, upstream from the confluence of the West Klinaklini River The West Klinaklini River is a brief but voluminous tributary of the Klinaklini River in British Columbia, Canada, joining it in its lower reaches above its mouth into Knight Inlet. Only 7 km long, it is formed by the meltwater from the Klina .... References * Canyons and gorges of British Columbia Pacific Ranges Central Coast of British Columbia {{BritishColumbiaCoast-geo-stub ...
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Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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Klinaklini River
The Klinaklini River ( Kwak'wala name T̓linat̓łina also spelled ƛ̓inaƛ̓ina) is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet. A different spelling of ''Klinaklini'' is Kleena Kleene, which is the name of a recreational community on the river just below its exit from the Pantheon Range onto the Chilcotin Plateau. In the area of Kleena Kleene the Klinaklini, Homathko and Chilanko River basins share the same stretch of plateau. The names Kleena Kleene and Klinaklini derive from the Kwak'wala word for eulachon grease, which is made from the eulachon, a small oily fish that ascend coastal rivers. There is a First Nation village of the Tanakteuk subdivision of the Kwakwaka'wakw peoples at the mouth of the river, Tsawatti. Located on the Indian Reserve of the same name, it is the primary eulachon fishing and preservati ...
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Pacific Ranges
, photo = Mount Garibaldi (50997016501).jpg , photo_size = 280px , photo_caption = Mount Garibaldi massif as seen from Squamish , map = , map_image = South BC-NW USA-relief PacificRanges.png , map_caption = Pacific Ranges as defined in S. Holland ''Landforms of British Columbia'' , map_relief = , map_size = 280px , highest = Mount Waddington , area_km2 = 108237 , elevation_m = 4019 , elevation_ref = , prominence_m = , prominence_ref = , isolation_km = , isolation_ref = , coordinates = , coordinates_ref = , location = British Columbia, Canada , parent = Coast Mountains , type = , age = , geology = , volcanic_arc = , volcanic_belt = , volcanic_field = , volcanic_arc/belt = , last_eruption = , embedded = The Pacific Ranges are the souther ...
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Coast Mountains
The Coast Mountains (french: La chaîne Côtière) are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia south to the Fraser River. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. The Coast Mountains are part of a larger mountain system called the Pacific Coast Ranges or the Pacific Mountain System, which includes the Cascade Range, the Insular Mountains, the Olympic Mountains, the Oregon Coast Range, the California Coast Ranges, the Saint Elias Mountains and the Chugach Mountains. The Coast Mountains are also part of the American Cordilleraa Spanish term for an extensive chain ...
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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 ...
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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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Knight Inlet
Knight Inlet (Kwakʼwala: ''Tsawatti'') is one of the principal inlets of the British Columbia Coast, and the largest of the major inlets in the southern part of the Coast. It is fifth in sequence of the great saltwater inlets north from the 49th parallel near Vancouver, but it is the first whose outflow points away from the Strait of Georgia, opening into Queen Charlotte Strait at the Kwakwakaʼwakw community of Memkumlis (often known by the name of the group who were based there, the Mamalilikala) on Village Island. Geography The inlet's opening lies east of Malcolm Island and the fishing town of Port McNeill on Vancouver Island, and just north of the opening of the upper end of Johnstone Strait, which separates Vancouver Island from the archipelago between it and the mainland. Knight Inlet is one of the longest on the BC Coast at about in length; it is about in average width. Its great volume of water causes a major current and severe turbulence at its mouth during tidal c ...
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West Klinaklini River
The West Klinaklini River is a brief but voluminous tributary of the Klinaklini River in British Columbia, Canada, joining it in its lower reaches above its mouth into Knight Inlet. Only 7 km long, it is formed by the meltwater from the Klinaklini Glacier, the main tongue of the vast Ha-Iltzuk Icefield (Silverthrone Glacier The Silverthrone Glacier is a glacier at the northwest head of Knight Inlet in southwestern British Columbia, Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the P ...), which lies west of the Klinaklini. References * Rivers of the Central Coast of British Columbia Rivers of the Pacific Ranges {{BritishColumbiaCoast-river-stub ...
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Canyons And Gorges Of British Columbia
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ...
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