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Brandywine Creek (British Columbia)
Brandywine Creek, also formerly known as the Long John River after a local prospector and trapper, is a tributary of the Cheakamus River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, entering that stream via Daisy Lake, just below Brandywine Falls. The creek is about 14 km in length and originates on the south slope of Brandywine Mountain in Brandywine Meadows, at the southern end of the Powder Mountain Icefield and is the next basin immediately southwest of that of the Callaghan Valley, the site of the Nordic events facility for the 2010 Olympics. The creek's valley has been partially logged. An unnamed hot spring lies in its upper reaches, near Mount Fee. Name The creek's name is derived from that of Brandywine Falls, which earned its name in the course of a wager over its height in which the wagers were a bottle of brandy and a bottle of wine. See also *Brandywine Mountain *Mount Cayley *Brandywine Creek (other) Brandywine Creek may re ...
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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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Callaghan Valley
The Callaghan Valley is located in the Sea to Sky Country of southwestern, British Columbia, in the Pacific Ranges of the Coast Mountains 90 km north of Vancouver. It was the home of the 2010 Winter Olympics's Whistler Olympic Park, the venue for the Nordic events of the Olympics, and adventure tourism operations includinCanadian Wilderness Adventures Geography The valley is the basin of Callaghan Creek, at the head of which is Callaghan Lake and associated provincial park. Midway down Callaghan Creek is the confluence of Madeley Creek, just above which on that creek is Alexander Falls, which lies just at a bridge on the road to Callaghan Lake. On its western perimeter is the Powder Mountain Icefield, and the potentially active volcano Mount Cayley, which lies at the valley's southwestern extremity. Mount Callaghan, at the head of the valley, is a dormant volcano because its last eruption was not as recent as Mount Cayley's, nor does it display hot spring or seismic activi ...
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Hot Springs Of British Columbia
Hot or the acronym HOT may refer to: Food and drink *Pungency, in food, a spicy or hot quality *Hot, a wine tasting descriptor Places *Hot district, a district of Chiang Mai province, Thailand ** Hot subdistrict, a sub-district of Hot District, Thailand ** Tha Kham, Chiang Mai, also known as Hot, a town in Hot District, Chiang Mai province, Thailand * Hot, Albania, a village in the Malësi e Madhe municipality, Shkodër County, Albania Music * H.O.T. pronounced "H. O. T.", (High-Five of Teenagers), a South Korean boy band *Hawaii Opera Theatre, an opera company in Honolulu, Hawaii * Hot (American vocal group), best known for 1977 hit "Angel in Your Arms" 1976–1980 *Hot 97, branding for hip-hop radio station WQHT in New York City Albums * ''Hot'' (Freda Payne album), 1979 * ''Hot'' (Half Japanese album), 1995 * ''Hot'' (Inna album) or the title song (see below), 2009 * ''Hot'' (James Brown album) or the title song (see below), 1976 * ''Hot'' (Mel B album), 2000 * ''Hot'' (Pa ...
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Sea-to-Sky Corridor
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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Brandywine Creek (other)
Brandywine Creek may refer to: Canada *Brandywine Creek (British Columbia), a tributary of the Cheakamus River United States *Brandywine Creek (Big Blue River), in Indiana * Brandywine Creek (St. Joseph River tributary), in Michigan *Brandywine Creek (Broken Sword Creek tributary), Crawford County, Ohio *Brandywine Creek (Cuyahoga River tributary), in Summit County, Ohio *Brandywine Creek (Quittapahilla Creek tributary), in Lebanon County, Pennsylvania *Brandywine Creek (Christina River tributary), in Chester County, Pennsylvania and New Castle County, Delaware **East Branch Brandywine Creek, in Chester County, Pennsylvania **West Branch Brandywine Creek, in Chester County, Pennsylvania *Brandywine Creek State Park, in New Castle County, Delaware *Battle of Brandywine Creek, during the American Revolutionary War (1777) See also *Brandywine (other) *Baranduin or Brandywine River, a river in Middle-earth in the fiction of J. R. R. Tolkien *Brandywine Falls (other) B ...
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Mount Cayley
Mount Cayley is an eroded but potentially active stratovolcano in the Pacific Ranges of southwestern British Columbia, Canada. Located north of Squamish, British Columbia, Squamish and west of Whistler, British Columbia, Whistler, the volcano resides on the edge of the Powder Mountain Icefield. It consists of massif that towers over the Cheakamus River, Cheakamus and Squamish River, Squamish river valleys. All major summits have elevations greater than , Mount Cayley being the highest at . The surrounding area has been inhabited by indigenous peoples of the Americas, indigenous peoples for more than 7,000 years while geothermal exploration has taken place there for the last four decades. Part of the Garibaldi Volcanic Belt, Mount Cayley was formed by subduction zone volcanism along the western margin of North America. Eruptive activity began about 4,000,000 years ago and has since undergone three stages of growth, the first two of which built most of the volcano. The ...
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Mount Fee
Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located south of Callaghan Lake and west of the resort town of Whistler. With a summit elevation of and a topographic prominence of , it rises above the surrounding rugged landscape on an alpine mountain ridge. This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies. The mountain consists of a narrow north-south trending ridge of fine-grained volcanic rock and small amounts of fragmental material. It is long and wide with nearly vertical flanks. Mount Fee has two main summits, the southern tower of which is the highest. The summits are separated by a U-shaped crevice that gives them a prominent appearance. Geology Mount Fee is one of the southernmost volcanoes in the Mount Cayley volcanic field. This volcanic zone forms the central portion of the larger Garibaldi Volcanic Belt, which extends from the Si ...
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Whistler Olympic Park
The Whistler Olympic Park is the location of the Nordic events facilities for the 2010 Winter Olympics and is located in the Madeley Creek basin in the Callaghan Valley, west of Whistler, British Columbia, Canada. The facility hosted the Biathlon at the 2010 Winter Olympics, biathlon, Cross-country skiing at the 2010 Winter Olympics, cross-country skiing, Nordic combined at the 2010 Winter Olympics, Nordic combined, and Ski jumping at the 2010 Winter Olympics, ski jumping. After the Olympics will remain a public facility, complementing the extensive wilderness trails and alpine routes already in use. Three temporary stadiums were built with a capacity for 12,000 spectators each (6,000 for the 2010 Winter Paralympics, Paralympics). The location is approximately 8 km from the junction of its access road with British Columbia Highway 99, Highway 99 and 14 km from the Whistler Olympic Village. The two year construction project saw, of cross country and biathlon trails, two ...
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Powder Mountain Icefield
The Powder Mountain Icefield, also called the Powder Mountain Icecap and the Cayley Icefield, is a glacial field in the Pacific Ranges of southwestern British Columbia, Canada, about west of Whistler and about north of Vancouver. On the west side of the icefield is the valley of the Squamish River, while on its east is the Callaghan Valley, which is the setting for the Nordic facilities for the 2010 Winter Olympics. The icefield is studded by several volcanic formations, including active Mount Cayley. Other summits are Powder Mountain, Brandywine Mountain and Mount Fee. Mount Callaghan, a dormant volcano, is just northeast of the icefield. Mount Brew is just to its south. Geology Numerous subglacial eruptions beneath the Powder Mountain Icefield have formed many distinctive subglacial volcanoes in the Mount Cayley volcanic field and contain abundant glass and fine-scale jointing from rapid cooling of lava, such as Ember Ridge and Slag Hill. Mineralogically, the volcanics rang ...
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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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Brandywine Mountain
Brandywine Mountain, , is a summit in the Powder Mountain Icefield of the Pacific Ranges of the Coast Mountains of southwestern British Columbia, Canada, about west of the resort town of Whistler, British Columbia, Whistler. Its name is derived from that of Brandywine Falls Provincial Park, Brandywine Falls, which was the result of a bet over the falls' height (with the wagers being a bottle of wine and a bottle of brandy). See also *Mount Fee *Mount Cayley *Mount Callaghan *Brandywine Creek (British Columbia), Brandywine Creek References

Two-thousanders of British Columbia Pacific Ranges New Westminster Land District {{BritishColumbiaCoast-geo-stub ...
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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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