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Squamish River
The Squamish River is a short but very large river in the Canadian province of British Columbia. Its drainage basin is in size. The total length of the Squamish River is approximately . Course The Squamish River drains a complex of basins in the Coast Mountains just north of Vancouver. Its flows generally south to the head of Howe Sound where the town of Squamish is located. The Squamish River originates at the toe of the Pemberton Icefield. As it flows south from the glacier, it is joined by several more glacier fed tributaries. About 21.8 km southwest of the source, the Squamish meets the Elaho River. The Elaho River, which is the largest tributary of the Squamish, actually has more volume than the Squamish where they join. After its confluence with the Elaho, the river moves southeast for another 24.8 km until its confluence with the Ashlu River, its second largest tributary. Another 16.4 km from there, it is met by the Cheakamus River, and 4.7 km further ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Pacific Ranges
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Cayley Volcanic Field
The Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching from the Pemberton Icefield to the Squamish River. It forms a segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia. Most of the MCVF volcanoes were formed during periods of volcanism under sheets of glacial ice throughout the last glacial period. These subglacial eruptions formed steep, flat-topped volcanoes and subglacial lava domes, most of which have been entirely exposed by deglaciation. However, at least two volcanoes predate the last glacial period and both are highly eroded. The field gets its name from Mount Cayley, a volcanic peak located at the southern end of the Powder Mountain Icefield. This icefield covers much of the central portion of the volcanic field and is one of the several glacial fields in the Pacific Ranges of the Coast Mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Barrier
The Barrier is a lava dam retaining the Garibaldi Lake system in southwestern British Columbia, Canada. It is over thick and about long where it impounds the lake. The area below and adjacent to The Barrier is considered hazardous due to the unstable lava formation. Formation The Barrier was formed about 15,000–12,000 years ago when large lava flows emanated from Clinker Peak on the west shoulder of Mount Price. The large lava flowed towards the Cheakamus River valley. At the time of eruption, the valley was filled by glacial ice. The lava flow was stopped by the ice and ponded, eventually cooling to form an ice-marginal lava flow. When the ice melted away, the ice-cooled lava-flow front formed a precipitous cliff; water ponded behind the lava dam, forming Garibaldi Lake. Rubble Creek boulder field The unstable lava formation of The Barrier has in the past unleashed several debris flows in the area below Garibaldi Lake. The most recent major landslide in 1855-1856 forme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Squamish Nation
The Squamish Nation, Sḵwx̱wú7mesh Úxwumixw () in Sḵwx̱wú7mesh Sníchim (Squamish language), is an Indian Act government originally imposed on the Squamish (''Sḵwx̱wú7mesh'') by the Federal Government of Canada in the late 19th century. The Squamish are Indigenous to British Columbia, Canada. Their band government comprises 8 elected councillors, serving four-year terms, with an elected band manager. Their main reserves are near the town of Squamish, British Columbia and around the mouths of the Capilano River, Mosquito Creek, and Seymour River on the north shore of Burrard Inlet in North Vancouver, British Columbia. History The 'Squamish Nation', is an amalgamation of different villages, which became reserves under the Indian Act which the Canadian government imposed on the Squamish people. The origin of the Squamish Nation dates back to the late 19th century, when missionaries and Canadian government officials created a puppet government under the Indian Act ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Squamish People
The Squamish people (Squamish language, Squamish: ''Skwxwú7mesh'' , historically transliterated as Sko-ko-mish) are an Indigenous peoples of the Pacific Northwest Coast, indigenous people of the Pacific Northwest Coast. Archaeological evidence shows they have lived in the area for more than a thousand years. In 2012, there was population of 3,893 band members registered with the Squamish Nation. Their language is the Squamish language or ''Sḵwx̱wú7mesh snichim'', considered a part of the Coast Salish languages, and is categorized as Language extinction, nearly extinct with just 10 fluent speakers as of 2010. The traditional territory is in the area now in southwestern British Columbia, Canada, and covers Point Grey as the southern border. From here, it continues northward to Roberts Creek, British Columbia, Roberts Creek on the Sunshine Coast (British Columbia), Sunshine Coast, up the Howe Sound. The northern part includes the Squamish River, Squamish, Cheakamus River, Cheaka ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of British Columbia Rivers
The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes that are "in-line" connecting upper tributaries of listed rivers, or at their heads. Arctic drainage Arctic Ocean via Mackenzie River drainage :''(NB Liard tributaries on Yukon side of border omitted)'' Liard River watershed * Liard River ** Petiewewtot River **Fort Nelson River *** Sahtaneh River ****Snake River ***Muskwa River ****Prophet River ***** Minaker River *****Besa River **** Tetsa River **** Chischa River ****Tuchodi River ***Sikanni Chief River ****Buckinghorse River ***Fontas River ** Dunedin River ** Beaver River **Toad River ***West Toad River *** Racing River *** Schipa River **Grayling River ** Trout River **Vents River ** Smith River ** Coal River ** Rabbit River *** Gundahoo River **Kechika River *** Red River ***Turnag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashlu River
Ashlu Creek is a short and swift river-like creek in British Columbia. It is a tributary of the Squamish River and enters it about 24.3 km northwest of Squamish. Course Ashlu Creek, often called the "Ashlu River" (due to its size) or "the Ashlu", begins at the outlet of an unnamed lake east of Mount Crerar. From there all the way to its mouth, it flows southeast. Starting at Ashlu Falls is 3.9 km long Ashlu Canyon has several big rapids and large drops making it one of the best kayaking locations in the area. It ends about 2.1 km above the river's mouth. Hydroelectricity A 49 megawatt run-of-river hydro installation below the canyon went online December 2009. A diversion weir 5 km above the power house feeds water down a bored tunnel to the site. It is owned by Innergex Renewable Energy and is expected to produce 265,000 MWh annually.http://www.innergex.com/en/ashlu-creek Tributaries Ashlu Creek's only major tributary is Tatlow Creek, which flow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elaho River
The Elaho River is a c.70 km long river beginning in the Coast Mountains northwest of the towns of Whistler and Pemberton, British Columbia. It is a tributary of the Squamish River and is known for its whitewater rafting and kayaking as well as for the intense alpine scenery lining its route. The Elaho is much larger than the Squamish River when it meets with it. The Elaho is often subject to flash flooding. Course The Elaho River originates at the outlet of an unnamed lake fed directly by the Elaho Glacier. The river starts off by flowing southeast for about 10.2 miles until its confluence with Marlow Creek, which flows from the Pemberton Icefield. The river turns south here and flows south here about 12.6 to its confluence with its largest tributary, Clendinning Creek. Between Marlow Creek and Clendinning Creek, the river flows through spectacular Elaho Canyon, a popular whitewater rafting section. From the Clendinning Creek confluence, the river continues south for a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vancouver
Vancouver ( ) is a major city in western Canada, located in the Lower Mainland region of British Columbia. As the List of cities in British Columbia, most populous city in the province, the 2021 Canadian census recorded 662,248 people in the city, up from 631,486 in 2016. The Greater Vancouver, Greater Vancouver area had a population of 2.6million in 2021, making it the List of census metropolitan areas and agglomerations in Canada#List, third-largest metropolitan area in Canada. Greater Vancouver, along with the Fraser Valley Regional District, Fraser Valley, comprises the Lower Mainland with a regional population of over 3 million. Vancouver has the highest population density in Canada, with over 5,700 people per square kilometre, and fourth highest in North America (after New York City, San Francisco, and Mexico City). Vancouver is one of the most Ethnic origins of people in Canada, ethnically and Languages of Canada, linguistically diverse cities in Canada: 49.3 percent of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
