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Daisy Lake (British Columbia)
Daisy Lake, also referred to as Daisy Lake Reservoir, is a reservoir on the Cheakamus River in the Sea to Sky Country, Sea to Sky Corridor of southwestern British Columbia, Canada, just south of the Whistler, British Columbia, Resort Municipality of Whistler and immediately north of the abandoned townsite of Garibaldi, British Columbia, Garibaldi (which until 1932 had been also named Daisy Lake). Daisy Lake Dam was built in 1957 with the reservoir created merging the former natural Daisy Lake and another named Shadow Lake. The reservoir supplies the 158MW Cheakamus Generating Station on the Squamish River via an 11 km tunnel bored beneath the mountain range dividing the two rivers.https://www.bchydro.com/content/dam/hydro/medialib/internet/documents/rev_reqs_bch/pdf/ippbc_1_081_05_01_att1_pdf.pdf There is a BC Hydro-operated recreation area just above the dam, and public campgrounds and picnic tables at Brandywine Falls Provincial Park, which is near the head of the lake. ...
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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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Reservoir
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam A dam is a barrier that stops or restricts the flow of surface water or underground streams ...
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Cheakamus River
The Cheakamus River (pron. CHEEK-a-mus) is a tributary of the Squamish River, beginning on the west slopes of Outlier Peak in Garibaldi Provincial Park upstream from Cheakamus Lake on the southeastern outskirts of the resort area of Whistler. The river flows into Cheakamus Lake before exiting it and flowing northwest until it turns south and enters Daisy Lake. Between the outlet of Daisy Lake and its mouth, much of its length is spent going through Cheakamus Canyon, where the river flows through swift rapids and even one good sized waterfall. The river flows south from the lake and through the canyon before joining the Squamish River at Cheekye, a few miles north of the town of Squamish. The river's name is an anglicization of the name of Chiyakmesh ("people of the fish weir"), a village of the Squamish people and a reserve of the Squamish Nation. The c. 70 km (c.44 mi) length of the Cheakamus is followed by British Columbia Highway 99 (the Sea-to-Sky Highway) an ...
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Sea To Sky Country
The Sea-to-Sky Corridor, often referred to as the Corridor or the Sea to Sky Country, is a region in British Columbia spreading from Horseshoe Bay through Whistler to the Pemberton Valley and sometimes beyond to include Birken and D'Arcy. From Whistler on up, the region overlaps with the older and more historic Lillooet Country, of which Squamish, at the region's centre, was once the southward extension in the days when it was the rail-port terminus from the Interior, via Lillooet, and accessible from the Lower Mainland only by sea. Most of the region is in the Squamish-Lillooet Regional District, although south of Britannia Beach a small part of the region is in the Greater Vancouver Regional District. The term "Corridor" refers to the alignment of the region's towns along Highway 99, also known as the Sea to Sky Highway, which links together the regions' three main centres - Squamish, Whistler and Pemberton. There is little development other than resource extraction out ...
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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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Whistler, British Columbia
Whistler ( Lillooet/Ucwalmícwts: Cwitima, ; Squamish/Sḵwx̱wú7mesh: Sḵwiḵw, ) is a resort municipality in Squamish-Lillooet Regional District, British Columbia, Canada. It is located in the southern Pacific Ranges of the Coast Mountains, approximately north of Vancouver and south of Pemberton. It has a permanent population of approximately 13,982 (2021), as well as a larger but rotating population of seasonal workers. Over two million people visit Whistler annually, primarily for alpine skiing and snowboarding and, in the summer, mountain biking at Whistler Blackcomb. Its pedestrian village has won numerous design awards, and Whistler has been voted among the top destinations in North America by major ski magazines since the mid-1990s. During the 2010 Winter Olympics, Whistler hosted most of the alpine, Nordic, luge, skeleton, and bobsled events. History The Whistler Valley is located around the pass between the headwaters of the Green River and the upper-mid ...
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Garibaldi, British Columbia
Garibaldi, originally named Daisy Lake and also known as Garibaldi Lodge and Garibaldi Townsite, is a locality and ghost town in British Columbia, Canada, on the Cheakamus River around its confluence with Rubble Creek and just south of Daisy Lake. The CN railway (formerly BC Rail) and British Columbia Highway 99 traverses it north–south. Although some buildings remain, including public works facilities, the community is now officially depopulated due to the geohazard posed by The Barrier, a lava dam holding back Garibaldi Lake that has let go at various points in the past; Rubble Creek, the source of which is Garibaldi Lake, gets its name from the large boulder field created by successive degenerations of The Barrier. History The townsite had come into existence shortly after the opening of the Pacific Great Eastern Railway, with its post office opening in 1916, and it had been the site of Garibaldi Lodge, one of several railway lodges along the rail line, the most well kn ...
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Daisy Lake Dam
Daisy, Daisies or DAISY may refer to: Plants * ''Bellis perennis'', the common daisy, lawn daisy or English daisy, a European species Other plants known as daisy * Asteraceae, daisy family ** ''Euryops chrysanthemoides'', African bush daisy ** ''Osteospermum'', African daisy ** ''Tetraneuris acaulis'', angelita daisy ** ''Melampodium leucanthum'', blackfoot daisy ** ''Glebionis coronaria'', crown daisy ** ''Brachyglottis greyi'', daisy bush ** ''Olearia'', daisy bush ** ''Argyranthemum'', dill daisy, marguerite daisy ** ''Rhodanthemum hosmariense'', Moroccan daisy ** ''Leucanthemum vulgare'', oxeye daisy, dog daisy ** ''Leucanthemum × superbum'', Shasta daisy ** ''Brachyscome'', several species ** ''Gerbera jamesonii'', Barberton daisy, Transvaal daisy ** ''Ismelia carinata'', tricolor daisy * ''Scabiosa prolifera'', Carmel daisy * ''Globularia'', globe daisies * ''Cleretum bellidiforme'', Livingstone daisy Arts, entertainment and media Film and television * Daisy (advertisement) ...
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Cheakamus Generating Station
Cheakamus is an anglicization of Chiyakmesh, the Skwxw7mesh language name for one of their villages, now located on Cheakamus Indian Reserve No. 11. Cheakamus may also refer to: *Cheakamus River * Cheakamus Lake *Cheakamus Powerhouse, on the Squamish River * ''Cheakamus'' (ship), see Union Steamship Company of British Columbia The Union Steamship Company of British Columbia was a pioneer firm on coastal British Columbia. It was founded in November 1889 by John Darling, a director of the Union Steamship Company of New Zealand, and nine local businessmen. The company beg ...
{{disambiguation, geo ...
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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 ...
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Brandywine Falls Provincial Park
Brandywine Falls Provincial Park is a provincial park in British Columbia, Canada, located adjacent to BC Highway 99 between Garibaldi and Whistler, British Columbia. It is managed by Sea to Sky Parks for BC Parks. Falls The falls are located on Brandywine Creek, which has its origin in the Powder Mountain Icefield to the west, and are formed by the lip of a lava flow flanking the west bank of the Cheakamus River. Just downstream of the falls is Daisy Lake. At least four basaltic lava flows of Late Pleistocene age comprise the vertical walls surrounding Brandywine Falls. These Cheakamus Valley basalts are part of the Garibaldi Volcanic Belt, a northwest-southeast chain of volcanoes and related lavas that form the northern end of the Cascade Volcanic Arc The Cascade Volcanoes (also known as the Cascade Volcanic Arc or the Cascade Arc) are a number of volcanoes in a volcanic arc in western North America, extending from southwestern British Columbia through Washington and Or ...
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Cheakamus Valley Basalts
The Cheakamus Valley basalts are a sequence of basaltic lava flows along the Cheakamus River in southwestern British Columbia, Canada. They are part of the Garibaldi section of the Cascade Volcanic Arc and were produced during an episode of volcanic eruptions from an unknown vent. The latest basaltic eruption deposited wood in lacustrine sediments under the lava flows that have been dated years old. These youngest lavas form isolated ridges above the older glaciated Cheakamus Valley basalts and were described as "esker-like" by Canadian volcanologist Bill Mathews. Columnar jointing is present all through the most recent basalt lava flow and pillow basalts exist in the lowermost unit, portions of which are underlain by hyaloclastite breccia. Bill Mathews suggested that these esker-like lava flows were deposited during subglacial eruptions that traveled away from the vent inside tunnels or trenches melted in the overlying ice sheet. Mathews based his suggestion on the age of the un ...
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