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Geography

Geography is the study of places, Earth’s physical features and environmental phenomena. Geographers also examine human populations and their impact on the natural world. This collection from The Canadian Encyclopedia covers a wide range of topics in both physical and human geography. These topics include geographic regions, sustainable development, and Indigenous populations.

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Gulf

A gulf is a body of water partly surrounded by land and connected to an ocean or sea. This connection sometimes takes the form of a narrow passage called a strait. The nomenclature of water inlets can be inconsistent between sources. Sometimes, the terms gulf,  bay and sea are used interchangeably. For example, the Arabian Sea and Hudson Bay can both be classified as gulfs. However, in most cases a gulf is deeper and larger than a bay and is also more enclosed from the ocean or sea to which it is connected. Because gulfs are partially surrounded by land, their waters are typically calmer than those of oceans. This makes them suitable for activities such as transportation, fishing and leisure.

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Geography of Quebec

The province of Quebec is composed of three of Canada’s sevenphysiographic regions. These regions are the St. Lawrence Lowlands, the Canadian Shield and the Appalachian region. The St. Lawrence Lowlands is the most fertile and developed region. The majority of the population of Quebec lives here, mainly between Montreal and Quebec City. The Canadian Shield covers most of Quebec from approximately 80 km north of the St. Lawrence River valley up to the Ungava region. It is a vast region composed of thousands of lakes and thousands of square kilometres of forested area. On the south bank of the St. Lawrence River, between the Richelieu River and the Gaspé Peninsula, is the Quebec part of the Appalachian mountain chain which extends from Gaspé south to Alabama.

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Plate Tectonics

Plate tectonics is the theory proposing that Earth’s outer rocky shell is divided into seven major and several smaller rigid plates. Forces generated by heat losses from the planet’s interior constantly move the plates about. Plate movements, ongoing over millions of years (see Geological History), open and close ocean basins, generate volcanoes, raise mountains, facilitate accumulation of mineral and petroleum deposits, and influence evolution and climate change. Friction between plates prevents steady motion and stores energy that is released in sudden movements, causing earthquakes.

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Geography of Alberta

Alberta is divided by three of Canada’s seven physiographic regions. These three regions are the Cordillera, Interior Plains and Canadian Shield. However, the vast majority of the province falls within the Interior Plains region. The Interior Plains may be further divided into prairie grassland, parkland and boreal forest. The prairie portion includes most of southern Alberta. This gently rolling grassland is relatively dry and mostly treeless. The parkland region predominates in central Alberta. This area varies from the flatland of old lake bottoms to rolling landscape with numerous lakes and depressions. The boreal forest region covers the northern half of the province. Here great rivers and lakes dominate the landscape, draining northward to the Arctic Ocean. In Alberta’s southwest corner an area of foothill ridges rise to the Rocky Mountains, forming part of Canada’s Cordillera region.

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Largest Cities in Canada by Population

Since the Second World War, Canadians have become increasingly urban, living primarily in cities. In an attempt to keep housing affordable, local governments have needed to balance burgeoning borders with urban density. Canada’s ten largest cities offer a glimpse at the many approaches and issues.

All populations are from the 2016 Canadian census and reflect the cities proper, as opposed to the larger census metropolitan area.

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Churchill River (Manitoba)

Churchill River, 1,609 km long, issues from Churchill Lake in northwestern Saskatchewan and flows southeast, east and northeast across the lowlands of northern Saskatchewan and Manitoba to Hudson Bay at Churchill, Manitoba. The name — for John Churchill, first duke of Marlborough and governor of the Hudson’s Bay Company from 1685 to 1691 — was applied to the river as early as 1686. The Cree called it Missinipi, meaning “great waters” or “big water.” (See also Longest Rivers in Canada.)

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Largest Lakes in Canada

Surveys suggest that there may be as many as 2 million lakes in Canada. While some look like small scratches on the country’s surface, many are quite large. Nearly fourteen per cent of the world’s lakes with surface areas over 500 km2 are located in Canada. Below is a list of the largest of these large lakes. The list is ordered by the lake’s total surface area, not just the portions within Canadian borders.

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Longest Rivers in Canada

Canada’s rivers have played a vital role in the country’s history and cultural heritage. As transportation routes for Indigenous people and early settlers, they connected the country before railways and other modes of transportation. They have also been a source of water, food and recreation for thousands of years. Below is a list of Canada’s 10 longest rivers. The list is ordered by the river’s total length, not just the portions within Canadian borders.

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Dam

A dam is a structure built across a waterway to control or stop the flow of water. This is called impounding the flow of water. Dams can be built by animals, such as beavers, or constructed by humans. In some cases, they are even formed by natural geological forces.

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Bay

A bay is a body of water partly surrounded by land and connected to a larger body of water. It is typically bigger than a cove and smaller than a gulf. However, this is not always the case. For example, Hudson Bay is much larger than the Persian Gulf. Strictly speaking and by international agreement, to be defined as a bay, a water body’s mouth (the boundary between itself and the larger body of water to which it is connected) must not exceed 24 nautical miles. In addition, its area must exceed that of a semicircle drawn with the mouth as its diameter.

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Dike

In geography and civil engineering, a dike is a barrier or ditch limiting or preventing the flow of water. Such barriers are also called levees. While a dam stretches across a waterway, a dike usually runs along its side. Dikes can form as a result of natural forces, but most are constructed by humans. The purpose of building a dike is usually to prevent flooding. New land can also be reclaimed by using dikes to drain wetlands or to push back the boundaries of a body of water.

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Camrose

Camrose, Alberta, incorporated as a city in 1955, population 18,742 (2016 census), 17,286 (2011 census). The city of Camrose, located 97 km southeast of Edmonton, is a distributing, medical, government and manufacturing centre for a rich, mixed-farming area.

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Cold Lake

Cold Lake, Alberta, incorporated as a city in 2000, population 14,961 (2016 census), 13,839 (2011 census). The city of Cold Lake is located on a lake of the same name, 290 km northeast of Edmonton. The  Cree called the lake “Kinosoo” or “big fish” after a Cree legend. European settlers named the lake for its deep, cold water.

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Vegreville

Vegreville, Alberta, incorporated as a town in 1906, population 5,708 (2016 census), 5,717 (2011 census). The town of Vegreville is located in the parkland region of east-central Alberta, 100 km east of Edmonton. It serves a rich agricultural region specializing in grains and some livestock.

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Raymond

Raymond, Alberta, incorporated as a town in 1903, population 3,708 (2016 census), 3,743 (2011 census). The town of Raymond is located in southern Alberta, approximately 35 km south of Lethbridge. In the early 1900s the area was settled by Mormons and Japanese labourers (see also Japanese Canadians). The Raymond Stampede, Canada’s first rodeo, has been held in the town since 1902.

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Causeway

A causeway is a raised path, railway or road across an expanse of low ground, wetlands or water. It is different from a bridge in that it has little or no opening underneath. Instead, it consists of a crest with embankments on either side. It is typically made of compacted earth, sand and rocks. In most cases, causeways are made by humans to connect different dry land areas to each other. Such connections can also be made up of a combination of causeway and bridge segments. Sometimes, a causeway can serve several purposes simultaneously. In addition to the passage it provides, the bulk of its structure may be intended to function as a dam or dike.