Brandywine Mountain
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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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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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New Westminster Land District
The New Westminster Land District is one of 59 land districts of British Columbia, Canada, which are the underlying cadastral divisions of that province, created with rest of those on Mainland British Columbia via the ''Lands Act'' of the Colony of British Columbia (1858–1866), Colony of British Columbia in 1860. The British Columbia government's BC Names system, a subdivision of GeoBC, defines a land district as "a territorial division with legally defined boundaries for administrative purposes". All land titles and surveys use the Land District system as the primary point of reference, and entries in BC Names for placenames and geographical objects are so listed. Description This land district is named for the city of New Westminster, which at the time of its creation was the capital of the Mainland Colony. Greater Vancouver, the Fraser Valley, the Sunshine Coast (British Columbia), Sunshine Coast and the Highway 99 corridor up to and including the Resort Municipality of Whi ...
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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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National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
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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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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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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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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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Bottle Of Wine
"Bottle of Wine" is a song written and recorded by Tom Paxton, which was also a hit for the band The Fireballs, whose version reached #9 on the ''Billboard'' Hot 100 in 1968 and #5 in Canada. It also reached #3 in South Africa. The song, which included only two of Paxton's four verses, with the chorus repeated, appeared on the band's 1967 album, ''Bottle of Wine''. The Fireballs' record was produced by Norman Petty, and was ranked #63 on ''Billboard'' magazine's Top ''Hot 100'' songs of 1968. Other versions *Judy Collins on her 1964 concert album ''The Judy Collins Concert''. *Tom Paxton's original was released on his 1965 album, ''Ain't That News!'' *The Kingston Trio covered the song on their 1965 album 'Stay Awhile' * Joe Brown released a single in 1968. *Sweeney's Men recorded it with the Capitol Showband in 1970. *Doc Watson and Merle Watson in 1973, which reached #71 on the U.S. country chart.
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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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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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