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			Happened to find this series of 6 
		videos and thought it would make an interesting introduction. 
		 Part 1: Kanada (BC 
		Canada) Vancouver 
		 
		Vancouver (/vænˈkuːvər/) is a coastal seaport city on the mainland of 
		British Columbia, Canada. The 2011 census recorded more than 603,000 
		people in the city, making it the eighth largest among Canadian 
		cities.The metropolitan area, with more than 2.3 million residents, is 
		the third most populous metropolitan area in the country and the most 
		populous in Western Canada. With 5,249 people per square kilometre 
		(13,590 per sq mile), the City of Vancouver is the most densely 
		populated of Canadian municipalities having more than 5,000 
		residents.Vancouver is one of the most ethnically and linguistically 
		diverse cities in Canada, with 52% for whom English is not their first 
		language. 
		 
		The settlement of Gastown grew to the West of the Hastings logging 
		sawmill established in 1867, enlarging to become the townsite of 
		Granville. With the announcement that the railhead would reach the site, 
		it was renamed "Vancouver" and incorporated as a city in 1886. By 1887, 
		the transcontinental railway was extended to the city to take advantage 
		of its large natural seaport, which soon became a vital link in a trade 
		route between the Orient, Eastern Canada, and London.As of 2009, Port 
		Metro Vancouver is the busiest and largest port in Canada, and the most 
		diversified port in North America.Vancouver is well known as an urban 
		centre surrounded by nature tourism is one of it's largest industry's. 
		Major film production studios in Vancouver and Burnaby have turned Metro 
		Vancouver into the third-largest film production centre in North America 
		after Los Angeles and New York City, earning it the film industry 
		nickname, Hollywood North. 
		Part 2: White Rock & Tofino Vancouver 
		Island 
		 
		White Rock is a city in British Columbia, Canada, that lies within the 
		Metro Vancouver regional district. It borders Semiahmoo Bay and is 
		surrounded on three sides by the City of Surrey, British Columbia. To 
		the south lies the Semiahmoo First Nation, which is within the city 
		limits of Surrey. Semiahmoo Bay and the Southern Gulf Islands in the 
		Strait of Georgia are also to the south. 
		 
		The boundaries between White Rock and Surrey are Bergstrom Road (136 
		Street) to the west, North Bluff Road (16th Avenue) to the north, Stayte 
		Road (160 Street) to the east, and 8th Avenue to the south. The area 
		south of 8 Avenue from Stayte Road westward to where 8 Avenue meets the 
		water is the Semiahmoo Indian Reserve and lies within the bounds of the 
		City of Surrey (though it is governed separately). The Surrey 
		neighbourhoods of Ocean Park and Crescent Beach lie immediately to the 
		northwest. 
		 
		White Rock pier on a warm August dayWhite Rock has a moderate climate, 
		with average daily high temperatures of 23 degrees Celsius in summer and 
		6 degrees Celsius in winter. Pilots accustomed to flying around the area 
		often refer to it as 'the hole in the sky', referring to the fact that 
		White Rock is often bright and sunny while the rest of the Lower 
		Mainland is covered by cloud. 
		 
		The pier and promenade are popular destinations, but do not allow dogs, 
		bicycles or skateboards. These areas are very busy during the warmer 
		summer months.  
		 
		Tofino is a district of about 1,876 residents on the west coast of 
		Vancouver Island, in British Columbia, Canada, located at the western 
		terminus of Highway 4, on the tip of the Esowista Peninsula, at the 
		southern edge of Clayoquot Sound.The settlement of Tofino first acquired 
		the name in 1909 with the opening of the Tofino Post Office, named in 
		association with Tofino Inlet nearby. Tofino Inlet was named in 1792 by 
		the Spanish commanders Galiano and Valdés, in honor of Admiral Vicente 
		Tofiño, under whom Galiano had learned cartography.A popular tourist 
		destination in the summer, Tofino's population swells to many times its 
		winter size. It attracts surfers, nature lovers, campers, whale 
		watchers, fishermen, or anyone just looking to be close to nature. In 
		the winter it is not as bustling, although many people visit Tofino and 
		the west coast to watch storms on the water. Close to Tofino is Long 
		Beach, a scenic and popular year-round destination, at the Pacific Rim 
		National Park Reserve. Nearby Maquinna Marine Provincial Park,with its 
		natural hot springs, is located about 45 kilometres (28 mi) north of 
		Tofino and is also a popular day-trip destination for tourists although 
		it is only reachable by boat or float plane. 
		 
		Part 3: Victoria, Capital city of BC / Chemainus First Nation 
		 
		Chemainus is a community on the east coast of Vancouver Island, British 
		Columbia, Canada. 
		 
		Founded as a logging town in 1858, the town is now famous for its 39 
		outdoor murals. This outdoor gallery has given birth to 300 businesses, 
		including a theatre, antiques dealers, and eateries. The tourist 
		industry stemming from the murals saved the town after its mill closed 
		in the early 1980s. A resident of Chemainus is known as a Chemainiac. 
		 
		Chemainus TheatreThe name "Chemainus" comes from the native shaman and 
		prophet "Tsa-meeun-is" (Broken Chest). Legend says that the man survived 
		a massive wound in his chest to become a powerful chief. His people took 
		his name to identify their community, Chemainus First Nation. 
		 
		The railroad arrived in the 1880s and by the early 1920s the town's 
		population had ballooned to 600 persons. Today, Chemainus has a 
		population of approximately 5,000. 
		 
		Chemainus Secondary School is located in the town, and serves as a 
		secondary school for students living in Chemainus, Crofton, and Saltair. 
		 
		A BC Ferry terminal is located in Chemainus, which provides service to 
		Thetis Island and Penelakut Island (previously Kuper). 
		 
		Canada Railroad later. Japanese, and later, east Indians blended their 
		cultures with Scots and Germans looking for riches in the mines and 
		staying to work in the forests and on fishing boats. And the beautiful 
		Cowichan Valley has been the home of The Original First Nations peoples 
		and their ancestors for countless generations, whose history and lives 
		have been interwoven since those first white settlers came to the area.
		 
		 
		Victoria is the capital city of British Columbia, Canada and is located 
		on the southern tip of Vancouver Island off Canada's Pacific coast. The 
		city has a population of about 80,017 within the metropolitan area of 
		Greater Victoria, which has a population of 344,615, the 15th most 
		populous Canadian metro region. 
		 
		Victoria is about 100 kilometres (62 miles) from BC's largest city of 
		Vancouver on the mainland. The city is about 100 kilometres (62 miles) 
		from Seattle by airplane, ferry, or the Victoria Clipper passenger-only 
		ferry which operates daily, year round between Seattle and Victoria and 
		40 kilometres (25 miles) from Port Angeles, Washington by ferry across 
		the Juan de Fuca Strait. 
		 
		Named after Queen Victoria of the United Kingdom and of the Dominion of 
		Canada, Victoria is one of the oldest cities in the Pacific Northwest, 
		with British settlement beginning in 1841. The city has retained a large 
		number of its historic buildings, in particular its two most famous 
		landmarks, the British Columbia Parliament Buildings (finished in 1897 
		and home of the Legislative Assembly of British Columbia) and the 
		Empress hotel (opened in 1908). The city's Chinatown is the second 
		oldest in North America after San Francisco's. The region's Coast Salish 
		First Nations peoples established communities in the area long before 
		non-native settlement, possibly several thousand years earlier, which 
		had large populations at the time of European exploration. Victoria, 
		like many Vancouver Island communities, continues to have a sizable 
		First Nations presence, composed of peoples from all over Vancouver 
		Island and beyond. 
		 
		Known as the "City of Gardens," Victoria is an attractive city and a 
		popular tourism destination with a thriving technology sector that has 
		risen to its largest revenue producing private industry.The city has a 
		large non-local student population, who come to attend the University of 
		Victoria, Camosun College, Royal Roads University, the Sooke Schools 
		International Program and the Canadian College of Performing Arts. 
		Victoria is also popular with retirees, who come to enjoy the temperate 
		and usually snow-free climate of the area as well as the usually relaxed 
		pace of the city. 
		 
		Part 4: Whistler Shannon Falls, Brohm Lake 
		 
		Whistler is a Canadian resort town in the southern Pacific Ranges of the 
		Coast Mountains in the province of British Columbia, Canada, 
		approximately 125 kilometres (78 mi) north of Vancouver. Incorporated as 
		the Resort Municipality of Whistler (RMOW), it has a permanent 
		population of approximately 9,965, plus a larger but rotating 
		"transient" population of workers, typically younger people from beyond 
		BC, notably from Australia and Europe. 
		Over two million people visit Whistler annually, primarily for alpine 
		skiing and snowboarding and, in 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, though freestyle skiing and all 
		snowboarding events were hosted at Cypress Mountain near Vancouver. 
		 
		The Whistler Valley is formed by the pass between the headwaters of the 
		Green River and the upper-middle reaches of the Cheakamus. It is flanked 
		by glaciated mountains on both sides; the Garibaldi Ranges on the side 
		that contains the ski mountains, and a group of ranges with no 
		collective name but which are part of the larger Pacific Ranges and are 
		essentially fore-ranges of the Pemberton Icefield. Although there are a 
		few other routes through the maze of mountains between the basin of the 
		Lillooet River just east, the Cheakamus-Green divide is the lowest and 
		most direct and naturally was the main trading route of the Squamish and 
		Lil'wat First Nations long before the arrival of Europeans. One Lil'wat 
		legend of the Great Flood says that before the deluge, the people lived 
		at Green Lake 
		 
		2010 Winter Olympics: 
		Whistler was the Host Mountain Resort of the Vancouver 2010 Winter 
		Olympic and Paralympic Games, the first time the IOC has bestowed that 
		designation on a community. Whistler hosted the alpine technical and 
		speed events, the sliding events at Fitzsimmons Creek, the Nordic events 
		in the nearby Callaghan Valley and all the Paralympic events except the 
		opening ceremonies, sledge hockey and wheelchair curling. The Whistler 
		Olympic and Paralympic Village (commonly referred to as the Athlete's 
		village) housed around 2,400 athletes, coaches, trainers and officials. 
		Post-games, the site has been turned into a new residential 
		neighbourhood. 
		 
		Black bear: 
		Whistler's urban landscape was specifically designed to accommodate the 
		natural environment, as well as to re-mediate a large garbage dump which 
		became today's Whistler Village which had been one of the main 
		non-natural feeding grounds for black bear in the valley. Since the 
		resort's development, black bear populations have gradually recovered, 
		coupled with the loss of pines due to multi-year drought conditions, 
		bears have begun seeking food in settled areas. Many of Whistler's bears 
		have learned to do things like open car doors or hold spring-closed 
		gates open so they can reach food. Most are relatively docile and few 
		bear-human incidents have been reported. Whistler residents are strongly 
		conservationist, and the official response has relied heavily on 
		behavior modification for both bears and people. Removal or killing are 
		last resorts. The techniques being used have been studied and adopted by 
		other municipalities with bear problems around the world. 
		 
		Part 5: Banff National Park, Emerald Lake, Lake Louise, Revelstoke 
		 
		Lake Louise is a hamlet in Alberta, Canada within Improvement District 
		No. 9 Banff (Banff National Park). It is named for the nearby Lake 
		Louise, which in turn was named after the Princess Louise Caroline 
		Alberta (1848--1939), the fourth daughter of Queen Victoria, and the 
		wife of John Campbell, the 9th Duke of Argyll, who was the Governor 
		General of Canada from 1878 to 1883. The province of Alberta is also 
		named for Princess Louise. 
		 
		Emerald Lake is one of the most admired destinations in Yoho National 
		Park, with an unmatched diversity of both activities and landscapes 
		suited to the enthusiastic traveler. It was discovered in 1882, when 
		famed mountain guide Tom Wilson was led lakeside while rounding up a 
		group of horses that had gone astray, and was immediately taken by the 
		vivid Emerald-coloured waters. 
		 
		Lake Emreald: 
		Here the vegetation is quite stunning, with several different 
		microclimates suiting a new collection of sensitive plant species, 
		making for some impressively delicate floral displays. The moist, shady 
		enclaves common to the Emerald Lake region make it one of the best 
		places to spot a variety of tiny, fragile wild orchids that survive only 
		in finely balanced conditions. If you're paying attention, you may be 
		rewarded with a Yellow Lady Slipper, Spotted Orchid, or Calypso 
		sighting. 
		 
		An Outing at Emerald Lake 
		The hike around the lake, clocking in at about an hour, is one of the 
		least strenuous but most rewarding in the park. An incredible breadth of 
		geological features can be viewed from the lake, including the 
		world-famous Burgess Shale fossil beds, the Michael glacier, and an 
		avalanche slope carpeted by meadows where moose often graze. 
		Emerald Lake is a fantastic place to see wildlife, as animals are drawn 
		to the important water source. Bald eagles, moose, and ospreys are a 
		common sight, as are waterfowl such as loons and mergansers.The vibrant 
		waters of Emerald LakeHiking isn't the only way to see Emerald Lake, 
		however. Canoe and rowboat rentals are available at Emerald Sports, as 
		are cross-country skis and snowshoes in the winter. Fishing at Emerald 
		Lake is also quite popular during the summer months. Swimming comes 
		highly recommended for the experience, but is not for the faint of 
		heart. The water is cold! The more leisurely delight of having lunch at 
		the lakeside patio does the trick for some, as well. Picnic areas and 
		the Emerald Sports gift shop are also easily found. 
		 
		Emerald Lake is easily accessible from Field by a 10-minute car ride, or 
		by biking or cross-country skiing along the Tally Ho trail, depending on 
		the season. Be sure to make a stop at the Natural Bridge viewpoint on 
		the way! 
		 
		Revelstoke; population 7,500 municipal est. 2005) is a city in 
		southeastern British Columbia, Canada. It is located 641 kilometers (398 
		mi) east of Vancouver, and 415 kilometers (258 mi) west of Calgary, 
		Alberta. The city is situated on the banks of the Columbia River just 
		south of the Revelstoke Dam and near its confluence with the 
		Illecillewaet River. East of Revelstoke are the Selkirk Mountains and 
		Glacier National Park, penetrated by Rogers Pass used by the 
		Trans-Canada Highway and the Canadian Pacific Railway. South of the 
		community down the Columbia River are the Arrow Lakes and the Kootenays. 
		West of the city is Eagle Pass through the Monashee Mountains and the 
		route to Shuswap Lake. 
		 
		Part 6: Rocky Mountains, Columbia icefields, Athabasca Glacier 
		 
		Rocky Mountains: 
		The Rocky Mountains (or the Rockies) are a major mountain range in 
		western North America. The Rocky Mountains stretch more than 3,000 miles 
		(4,830 km) from the northernmost part of British Columbia, in western 
		Canada, to New Mexico, in the southwestern United States. Within the 
		North American Cordillera, the Rockies are somewhat distinct from the 
		Pacific Coast Ranges and the Cascade Range and Sierra Nevada which all 
		lie further to the west. 
		The Rocky Mountains were formed from 80 million to 55 million years ago 
		by the Laramide orogeny. Since then, erosion by water and glaciers have 
		sculpted the mountain range into dramatic valleys and peaks. At the end 
		of the last ice age, humans started to inhabit the mountain range. After 
		Europeans, such as Sir Alexander MacKenzie and the Lewis and Clark 
		expedition, started to explore the range, minerals and furs drove the 
		initial economic exploitation of the mountains, although the range 
		itself never became densely populated. 
		 
		Currently, much of the mountain range is protected by public parks and 
		forest lands, and is a popular tourist destination, especially for 
		hiking, camping, mountaineering, fishing, hunting, mountain biking, 
		skiing, and snowboarding. 
		 
		Athabasca Glacier: 
		The Columbia Icefield is an icefield located in the Canadian Rockies, 
		astride the Continental Divide of North America. The icefield lies 
		partly in the northwestern tip of Banff National Park and the southern 
		end of Jasper National Park. It is about 325 km² in area, 100 to 365 
		metres (328 to 1,197 ft) in depth and receives up to seven metres (275 
		in) of snowfall per year. The icefield feeds eight major glaciers, 
		including: 
		Athabasca Glacier,Castleguard Glacier,Columbia Glacier,Dome 
		Glacier,Stutfield Glacier,Saskatchewan Glacier 
		Some of the highest mountains in the Canada Rockies are located around 
		the edges: 
		Mount Andromeda (3,450 m),Mount Athabasca (3,491 m),Mount Bryce (3,507 
		m),Castleguard Mountain (3,090 m),Mount Columbia (3,747 m),Mount King 
		Edward (3,490 m),Mount Kitchener (3,505 m),North Twin Peak (3,684 
		m),South Twin Peak (3,566 m),Snow Dome (3,456 m),Stutfield Peak (3,450 
		m) 
		 
		Parts of the Icefield are visible from the Icefields Parkway. The 
		Athabasca Glacier has receded significantly since its greatest 
		modern-era extent in 1844. During the summer months visitors to the area 
		can travel onto the glacier in the comfort of large "snowcoaches". The 
		Columbia Icefield is also a major destination for ski mountaineering in 
		the winter months. 
		 
		The icefield was first reported in 1898 by J. Norman Collie and Hermann 
		Woolley after they had completed the first ascent of Mount Athabasca. 
		 
		The Athabasca River and the North Saskatchewan River originate in the 
		Columbia Icefield, as do tributary headwaters of the Columbia River.[1] 
		As the icefield is atop a triple Continental Divide these waters flow 
		ultimately north to the Arctic Ocean, east to Hudson Bay (and thence to 
		the North Atlantic Ocean), and south and west to the Pacific Ocean. 
		Hudson Bay, in some watershed divisions, is considered to be in the 
		Arctic watershed, in which case this would arguably not be a triple 
		continental divide point. 
		 
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