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Displaying 141-160 of 170 results
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Rideau River

The Rideau River flows 100 km northwards from the Rideau Lakes in eastern Ontario to the Ottawa River at Ottawa.

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Sable Island

Shaped like an open crescent, 35 km long and 1.6 km wide at its widest point, it narrows at both ends to West and East Spits, which continue offshore as shallow submerged bars.

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Banks Island

Banks Island, 70 028 km2, fifth-largest island in Canada, is the westernmost island of the Arctic Archipelago.

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Ocean

The interplay of these ocean waters with freshwater runoff from land creates the conditions that support large biological production on Canada's continental shelves and embayments (see COASTAL LANDFORM; DRAINAGE BASIN).

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Rocky Mountain Trench

The Rocky Mountain Trench is a long and deep valley extending approximately 1,500 km from the Bitterroot Valley in northwest Montana through British Columbia to the Liard Plain just south of the Yukon Territory. Its predominantly flat floor is 3–20 km wide and ranges in elevation between 600 m and 1,000 m above sea level. With walls made of sedimentary, volcanic and igneous rock, the Trench is sometimes referred to as the “Valley of a Thousand Peaks” because of the towering mountain ranges on either side: the Rocky Mountains to the east and the Columbia, Omineca and Cassiar mountains to the west. Humans have relied on the rich resources provided by this distinctive landscape from pre-colonial times to the present.

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Bow River

​The Bow River runs through the most populated region of Alberta, intersecting cities such as Banff, Canmore, Cochrane and Calgary.

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Red River

The Red River (880 km long) begins at the confluence of the Bois de Sioux and Otter Tail rivers at the border between Minnesota and North Dakota. It then flows north through southern Manitoba and into Lake Winnipeg. The last 175 km of the Red River, the portion located in Manitoba, is designated as a Canadian Heritage River due to its cultural and historical value. The Red River flows through a productive agricultural region that is prone to both drought and severe flooding — the largest flood in the area in recent history, coined “the flood of the century,” occurred in 1997. The river’s basin was once the bottom of a glacial lake, Lake Agassiz, which covered the region 8,000 years ago. Currently, the Red River provides water for municipal, industrial and agricultural uses, and offers numerous summer and winter recreational opportunities, including boating, fishing (including ice fishing), camping and skating.

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Beaufort Sea

The Beaufort Sea coast is low lying and subject to considerable scouring by ice and erosion by storm surges. The Canadian shelf and the Yukon/Alaskan shelf form the southern boundary of the Beaufort Sea, but they have significantly different widths and alignments.

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Niagara Falls (Waterfalls)

 The falls have eroded the soft shales and limestones of the escarpment at an average rate of 1.2 m per year and now stand 11 km from their place of origin at present-day QUEENSTON. Their recession rate has been variable though, as the volume of water flowing from the upper Great Lakes controls it.

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Cypress Hills

Ranching became important in the area after the Canadian Pacific Railway arrived at MAPLE CREEK in 1883. Beginning in 1906, part of the Cypress Hills was protected as a federal forest reserve. RESOURCE RIGHTS were transferred to the provinces in 1930.

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Rocky Mountains

Castlelike mountain resorts built on the rail line at Banff and Lake Louise have become all-season recreation centres for Banff National Park's (established 1885) many alpine attractions, which attract 4.5 million visitors annually.

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Canadian Shield

The Canadian Shield refers to the exposed portion of the continental crust underlying the majority of North America. The crust, also known as the North American Craton, extends from northern Mexico to Greenland and consists of hard rocks at least 1 billion years old. With the exception of the Canadian Shield, the rocks of the North American Craton are buried deep within the continent and covered by soil and other material. At 5 million km2, the Shield makes up roughly 50 per cent of Canada’s land mass. Shaped like a horseshoe — or the shields carried during hand-to-hand combat — the Canadian Shield extends from Labrador in the east to include nearly all of Québec, much of Ontario and Manitoba, the northern portion of Saskatchewan, the northeast corner of Alberta, much of the Northwest Territories and Nunavut and into the Arctic Archipelago. (It also reaches into parts of the United States, in New York, Wisconsin and Minnesota.) While at times a barrier to settlement, the Shield has also yielded great resources, including minerals, coniferous forests and the capacity for hydroelectric developments.

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Desert

The paucity of precipitation in deserts is due to one or a combination of causes.

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Laurentian Highlands

Although the other limits are less well defined, the highlands may be considered to extend 100-200 km northward from the scarps and to stretch from the Gatineau River in the west (mean elevation 400 m) some 550 km to the SAGUENAY RIVER in the northeast.

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Northwest Coast

 The Northwest Coast was the name given by 18th-century navigators and traders to the great arc of Pacific coast and offshore islands stretching from present-day northern California to an ill-defined point along the Alaska coast - at Prince William Sound or even Cook Inlet.

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Okanagan Lake

Okanagan Lake is located in the southern interior of British Columbia and is the largest lake in the Okanagan Valley.