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Geography of Canada

Canada has a vast geography that occupies much of the continent ofNorth America, sharing aland border with thecontiguous United States to the south and the U.S. state ofAlaska to the northwest. Canada stretches from theAtlantic Ocean in the east to thePacific Ocean in the west; to the north lies theArctic Ocean.[1]Greenland is to the northeast with a shared border onHans Island. To the southeast Canada shares amaritime boundary with France'soverseas collectivity ofSaint Pierre and Miquelon, the last vestige ofNew France.[2] By total area (including its waters), Canada is thesecond-largest country in the world, after Russia. By land area alone, however, Canadaranks fourth, the difference being due to it having the world's largest proportion of fresh water lakes.[3] Of Canada'sthirteen provinces and territories, only two are landlocked (Alberta andSaskatchewan) while the other eleven all directly border one of three oceans.

Geography of Canada
ContinentNorth America
RegionNorthern America
Coordinates60°00′N95°00′W / 60.000°N 95.000°W /60.000; -95.000
AreaRanked 2nd
 • Total9,984,671 km2 (3,855,103 sq mi)
 • Land91.08%
 • Water8.92%
Coastline243,042 km (151,019 mi)
Borders8,893 km
Highest pointMount Logan,
5,959 m (19,551 ft)
Lowest pointAtlantic Ocean, Sea Level
Longest riverMackenzie River,
4,241 km (2,635 mi)
Largest lakeGreat Bear Lake
31,153 km2 (12,028 sq mi)
Climatetemperate, orhumid continental tosubarctic orarctic in north, andtundra in mountainous areas, and the far north
Terrainmostlyplains andmountains in west, to highlands (low mountains) in the south east, and east, to flatlands in theGreat lakes
Natural resourcesiron ore,nickel,zinc, copper, gold, lead,molybdenum,potash,diamonds, silver, fish, timber,wildlife, coal, petroleum, natural gas,hydropower
Natural hazardspermafrost,cyclonic storms,tornadoes, earthquakes,forest fires
Environmental issuesair andwater pollution,acid rains
Exclusive economic zone5,599,077 km2 (2,161,816 sq mi)

Canada is home to the world's northernmost settlement,Canadian Forces Station Alert, on the northern tip ofEllesmere Island—latitude 82.5°N—which lies 817 kilometres (508 mi) from the North Pole.[4] Much of theCanadian Arctic is covered by ice andpermafrost.[5] Canada hasthe longest coastline in the world, with a total length of 243,042 kilometres (151,019 mi);[6] additionally,its border with the United States is the world's longest land border, stretching 8,891 kilometres (5,525 mi).[7] Three of Canada'sArctic islands,Baffin Island,Victoria Island andEllesmere Island, are among the ten largest in the world.[8]

Canada can be divided into seven physiographic regions: theCanadian Shield, theinterior plains, theGreat Lakes-St. Lawrence Lowlands, theAppalachian region, theWestern Cordillera,Hudson Bay Lowlands and theArctic Archipelago.[9] Canada is also divided intofifteen terrestrial and five marine ecozones,[10] encompassing over 80,000 classified species of life.[11] Since the end of the lastglacial period, Canada has consisted ofeight distinct forest regions, including extensiveboreal forest on theCanadian Shield;[12] 42 percent of the land acreage of Canada is covered by forests (approximately 8 percent of the world's forested land), made up mostly ofspruce,poplar andpine.[13] Canada has over 2,000,000 lakes—563 greater than 100 km2 (39 sq mi)—which is more than any other country, containing much of the world'sfresh water.[14][15] There are also freshwater glaciers in theCanadian Rockies, theCoast Mountains and theArctic Cordillera.[16] A recent globalremote sensing analysis also suggested that there were 6,477 km2 of tidal flats in Canada, making it the 5th ranked country in terms of how much tidal flat occurs there.[17]Protected areas of Canada andNational Wildlife Areas have been established to preserve ecosystems.[18]

Canada is geologically active, having many earthquakes and potentially active volcanoes, notably theMount Meager massif,Mount Garibaldi,Mount Cayley, and theMount Edziza volcanic complex.[19] Average winter and summer hightemperatures across Canada range fromArctic weather in the north, to hot summers in the southern regions, with four distinct seasons.

Physiography

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Canada can be divided into seven physiographic regions: theCanadian Shield, theinterior plains, theGreat Lakes-St. Lawrence Lowlands, theAppalachian region, theWestern Cordillera,Hudson Bay Lowlands, and theArctic Archipelago.

Canada covers 9,984,670 km2 (3,855,100 sq mi) and a panoply of various geoclimatic regions, of which there are seven main regions.[9] Canada also encompasses vast maritime terrain, with the world's longest coastline of 243,042 kilometres (151,019 mi).[20] Thephysical geography of Canada is widely varied.Boreal forests prevail throughout the country, ice is prominent innortherly Arctic regions and through theCanadian Rocky Mountains, and the relatively flatCanadian Prairies in the southwest facilitate productive agriculture.[21] TheGreat Lakes feed theSt. Lawrence River (in the southeast) where lowlands host much of Canada's population.

TheNational Topographic System is used byNatural Resources Canada for providing general purposetopographic maps of the country. 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.[22] These maps are used by all levels of government and industry forforest fire andflood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning.[22]

Appalachian Mountains

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TheAppalachian mountain range extends fromAlabama insouthern United States through theGaspé Peninsula and theAtlantic Provinces, creating rolling hills indented by river valleys.[23] It also runs through parts of southernQuebec.[23]

The Appalachian Mountains (more specifically theChic-Choc,Notre Dame, andLong Range Mountains) are an old and eroded range of mountains, approximately 380 million years in age. Notable mountains in the Appalachians includeMount Jacques-Cartier (Quebec, 1,268 m or 4,160 ft),Mount Carleton (New Brunswick, 817 m or 2,680 ft),The Cabox (Newfoundland, 814 m or 2,671 ft).[24] Parts of the Appalachians are home to a richendemic flora and fauna and are considered to have beennunataks during the lastglaciation era.

Great Lakes and St. Lawrence Lowlands

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A map of theGreat Lakes Basin showing the five sub-basins within. Left to right they are:Superior, includingNipigon's basin, (magenta);Michigan (cyan);Huron (pale green);Erie (yellow);Ontario (light coral).

TheGreat Lakes-St. Lawrence Lowlands, or simply St. Lawrence Lowlands, is aphysiographic region ofEastern Canada that comprises a section of southernOntario bounded on the north by theCanadian Shield and by three of theGreat LakesLake Huron,Lake Erie andLake Ontario — and extends along theSt. Lawrence River to theStrait of Belle Isle[25] and theAtlantic Ocean. The lowlands comprise three sub-regions that were created by intrusions from adjacent physiographic regions — the West Lowland, Central Lowland and East Lowland.[25] The West Lowland includes theNiagara Escarpment, extending from theNiagara River to theBruce Peninsula andManitoulin Island.[25] The Central Lowland stretches between theOttawa River and the St. Lawrence River.[25] The East Lowland includesAnticosti Island,Îles de Mingan, and extends to the Strait of Belle Isle.

 
St. Lawrence Lowlands,Sainte-Anne river, rang du Rapide-Sud,Saint-Casimir

The St. Lawrence Lowlands is one of the most densely populated, prosperous and productive regions inCanada. Major urban areas includeToronto,Montreal,Ottawa-Gatineau andQuebec City.

The St. Lawrence Lowlands was covered bysurficial deposits left byice sheets following thePleistocene glaciations.[25] It is the smallest of Canada's seven physiographic regions — the others being theArctic Lands, theCordillera, theInterior Plains, theCanadian Shield, theHudson Bay Lowlands and theAppalachian Uplands — distinguished by topography and geology.[25] The boundaries of the area largely reflect that of theMixedwood Plains Ecozone, the smallest of Canada's fifteen terrestrialecozones.

Canadian Shield

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Further information:Canadian Shield
 
TheCanadian Shield is a broad region of Precambrian rock (pictured in shades of red)

The northeastern part ofAlberta, northern parts ofSaskatchewan,Manitoba, Ontario and Quebec, all ofLabrador and theGreat Northern Peninsula ofNewfoundland, eastern mainlandNorthwest Territories, most ofNunavut's mainland and, of itsArctic Archipelago,Baffin Island and significant bands through Somerset, Southampton, Devon and Ellesmere islands are located on a vastrock base known as theCanadian Shield.[26] The Shield mostly consists of eroded hilly terrain and contains many lakes and important rivers used forhydroelectric production, particularly in northern Quebec and Ontario. The Shield also encloses an area ofwetlands around theHudson Bay. Some particular regions of the Shield are referred to asmountain ranges, including theTorngat andLaurentian Mountains.[27]

The Shield cannot support intensive agriculture, although there is subsistence agriculture and small dairy farms in many of the river valleys and around the abundant lakes, particularly in the southern regions.Boreal forest covers much of the shield, with a mix ofconifers that provide valuable timber resources in areas such as theCentral Canadian Shield forestsecoregion that covers much ofNorthern Ontario.

The Canadian Shield is known for its vastmineral reserves such asemeralds,diamonds andcopper, and is there also called the "mineral house".[27]

Canadian Interior Plains

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Further information:Interior Plains
 
Palliser's Triangle, delineating prairie soil types in thePrairie provinces.

TheCanadian Prairies (usually referred to as simply the Prairies in Canada) is a region inWestern Canada. It includes the Canadian portion of theGreat Plains and the Prairie provinces, namelyAlberta,Saskatchewan, andManitoba.[28] These provinces are partially covered bygrasslands,plains, andlowlands, mostly in the southern regions. The northernmost reaches of the Canadian Prairies are less dense in population, marked byforests and more variabletopography.[29] If the region is defined to include areas only covered byprairie land, the corresponding region is known as theInterior Plains.[30] Physical or ecological aspects of the Canadian Prairies extend to northeasternBritish Columbia, but that area is not included in political use of the term.[31]

The prairies in Canada are abiome oftemperate grassland andshrubland within the prairieecoregion of Canada that consists ofnorthern mixed grasslands in Alberta, Saskatchewan,southern Manitoba, as well asnorthern short grasslands in southeastern Alberta and southwestern Saskatchewan.[32] ThePrairies Ecozone of Canada includes thenorthern tall grasslands in southern Manitoba andAspen parkland, which coverscentral Alberta, central Saskatchewan, and southern Manitoba.[33] The Prairie starts from north ofEdmonton and it covers the three provinces in a southward-slanting line east to the Manitoba–Minnesota border.[34] Alberta has the most land classified as prairie, while Manitoba has the least, as theboreal forest begins more southerly in Manitoba than in Alberta.[35]

Canadian Arctic

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Main article:Arctic Archipelago

While the largest part of the Canadian Arctic is composed of seemingly endlesspermafrost andtundra north of thetree line, it encompasses geological regions of varying types: theArctic Cordillera (with theBritish Empire Range and theUnited States Range onEllesmere Island) contains the northernmost mountain system in the world. TheArctic Lowlands and Hudson Bay lowlands comprise a substantial part of the geographic region often designated as the Canadian Shield (in contrast to the sole geologic area). The ground in the Arctic is mostly composed of permafrost, making construction difficult and often hazardous, and agriculture virtually impossible.[36]

The Arctic, when defined as everything north of the tree line, covers most ofNunavut and the northernmost parts of Northwest Territories,Yukon, Manitoba, Ontario, Quebec and Labrador. The archipelago consists of 36,563 islands, of which 94 are classified as major islands, being larger than 130 km2 (50 sq mi), and cover a total area of 1,400,000 km2 (540,000 sq mi).[36]

Western Cordillera

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Further information:Pacific Cordillera (Canada)
 
Map of theHart Ranges in British Columbia

TheCoast Mountains inBritish Columbia run from the lowerFraser River and theFraser Canyon northwestward, separating theInterior Plateau from the Pacific Ocean.[37] Its southeastern end is separated from theNorth Cascades by theFraser Lowland, where nearly a third ofWestern Canada's population reside.

The coastal flank of the Coast Mountains is characterized by an intense network offjords and associated islands, very similar to theNorwegian coastline inNorthern Europe; while their inland side transitions to the highplateau withdryland valleys notable for a series of largealpine lakes similar to those in southernSwitzerland, beginning in deep mountains and ending in flatland. They are subdivided in three main groups, thePacific Ranges between the Fraser River andBella Coola, theKitimat Ranges from there northwards to theNass River, and theBoundary Ranges from there to the mountain terminus in Yukon atChampagne Pass andChilkat Pass northwest ofHaines, Alaska.[37] TheSaint Elias Mountains lie to their west and northwest, while theYukon Ranges and Yukon Basin lie to their north. On the inland side of the Boundary Ranges are theTahltan andTagish Highlands and also theSkeena Mountains, part of theInterior Mountains system, which also extend southwards on the inland side of theKitimat Ranges.[37]

The terrain of the main spine of the Coast Mountains is typified by heavyglaciation, including several very largeicefields of varying elevation. Of the three subdivisions, the Pacific Ranges are the highest and are crowned byMount Waddington, while the Boundary Ranges contain the largest icefields, theJuneau Icefield being the largest. The Kitimat Ranges are lower and less glacier-covered than either of the other two groupings, but are extremely rugged and dense.

The Coast Mountains are made ofigneous andmetamorphic rock from an episode ofarc volcanism related tosubduction of theKula andFarallon Plates during theLaramide orogeny about 100 million years ago.[38] The widespreadgranite forming the Coast Mountains formed when magma intruded and cooled at depth beneath volcanoes of theCoast Range Arc whereas the metamorphic formed when intruding magma heated the surrounding rock to produceschist.

TheInsular Mountains extend fromVancouver Island in the south to theHaida Gwaii in the north on theBritish Columbia Coast. It contains two main mountain ranges, theVancouver Island Ranges on Vancouver Island and theQueen Charlotte Mountains on Haida Gwaii.[39]

Hudson Bay Lowlands

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The Hudson Bay Lowlands approximately coincide with theSouthern Hudson Bay taigaecoregion of North America.

TheHudson Bay Lowlands is a vastwetland located between theCanadian Shield and southern shores ofHudson Bay andJames Bay. Most of the area lies within the province ofOntario, with smaller portions reaching intoManitoba andQuebec. Many wide and slow-movingrivers flow through this area toward the saltwater of Hudson Bay: these include theChurchill,Nelson andHayes in Manitoba,Severn,Fawn,Winisk, Asheweig,Ekwan,Attawapiskat, andAlbany in Ontario, and theHarricana,Rupert andEastmain in Quebec.[40] This is the largest wetland in Canada, and one of the largest in the world.[41] The region can be subdivided into three bands running roughly northwest to southeast: the Coastal Hudson Bay Lowland (a narrow band along the northern coast),[42] Hudson Bay Lowland (a broader band extending to slightly south of the Ekwan River),[43] and James Bay Lowland (all the rest of the southern/eastern lands, making up close to 50% of the total Lowlands area).[44]

The entire area was covered by ice during the lastglaciation, and thepeatlands have accumulated over the last ten thousand years. Plants from the boreal forest mix with arctic species.[45] A majority of the wetland is peat bog and fen, although salt marshes occur along the coast, and marshes andwet meadows occur along the major rivers. The wetlands provide important habitat for migratory birds including shorebirds (e.g.,yellow rail) and waterfowl (e.g.,snow geese). Large mammals includepolar bears andwolverines.[41]

Extreme points

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Topographic map

The northernmost point of land within the boundaries of Canada isCape Columbia,Ellesmere Island,Nunavut83°06′40″N69°58′19″W / 83.111°N 69.972°W /83.111; -69.972 (Cape Columbia, Nunavut).[46] The northernmost point of the Canadian mainland isZenith Point onBoothia Peninsula, Nunavut72°00′07″N94°39′18″W / 72.002°N 94.655°W /72.002; -94.655 (Zenith Point, Nunavut).[46] The southernmost point isMiddle Island, inLake Erie, Ontario (41°41′N 82°40′W); the southernmost water point lies just south of the island, on the Ontario–Ohio border (41°40′35″N). The southernmost point of the Canadian mainland isPoint Pelee, Ontario41°54′32″N82°30′32″W / 41.909°N 82.509°W /41.909; -82.509 (Point Pelee, Ontario).[46] The lowest point is sea level at 0 m,[47] whilst the highest point isMount Logan,Yukon, at 5,959 m / 19,550 ft60°34′01″N140°24′18″W / 60.567°N 140.405°W /60.567; -140.405 (Mount Logan, Yukon).[46]

The westernmost point isBoundary Peak 187 (60°18′22.929″N 141°00′7.128″W) at the southern end of theYukonAlaska border, which roughly follows 141°W but leans very slightly east as it goes North60°18′04″N141°00′36″W / 60.301°N 141.010°W /60.301; -141.010 (Boundary Peak 187).[48][46] The easternmost point isCape Spear, Newfoundland (47°31′N 52°37′W)47°31′23″N52°37′08″W / 47.523°N 52.619°W /47.523; -52.619 (Cape Spear, Newfoundland).[46] The easternmost point of the Canadian mainland is Elijah Point,Cape St. Charles, Labrador (52°13′N 55°37′W)52°13′01″N55°37′16″W / 52.217°N 55.621°W /52.217; -55.621 (Elijah Point, Labrador).[46]

The Canadianpole of inaccessibility is allegedly near Jackfish River,Alberta (59°2′N 112°49′W).[49] The furthest straight-line distance that can be travelled to Canadian points of land is between the southwest tip ofKluane National Park and Reserve (next toMount Saint Elias) and Cripple Cove,Newfoundland (nearCape Race) at a distance of 3,005.60 nautical miles (5,566.37 km; 3,458.78 mi).

Climatology

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Further information:Temperature in Canada
 
Köppen climate classification types of Canada

Climate varies widely from region to region. Winters can be harsh in many parts of the country, particularly in the interior and Prairie provinces, which experience acontinental climate, where daily average temperatures are near −15 °C (5 °F), but can drop below −40 °C (−40 °F) with severewind chills.[50] In non-coastal regions, snow can cover the ground for almost six months of the year, while in parts of the north snow can persist year-round. Coastal British Columbia has a temperate climate, with a mild and rainy winter. On the east and west coasts, average high temperatures are generally in the low 20s °C (70s °F), while between the coasts, the average summer high temperature ranges from 25 to 30 °C (77 to 86 °F), with temperatures in some interior locations occasionally exceeding 40 °C (104 °F).[51]

Much ofNorthern Canada is covered by ice andpermafrost; however, the future of the permafrost is uncertain because the Arctic has been warming at three times the global average as a result ofclimate change in Canada.[52] Canada's annual average temperature over land has warmed by 1.7 °C (3.1 °F), with changes ranging from 1.1 to 2.3 °C (2.0 to 4.1 °F) in various regions, since 1948.[53] The rate of warming has been higher across the North and in the Prairies.[53] In the southern regions of Canada,air pollution from both Canada and the United States—caused by metal smelting, burning coal to power utilities, and vehicle emissions—has resulted inacid rain, which has severely impacted waterways, forest growth andagricultural productivity in Canada.[54]

Biogeography

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Main article:Wildlife of Canada
 
ELC Ecozones and ecoprovinces of Canada

Canada is divided into fifteen major terrestrial and five marine ecozones, that are further subdivided into 53ecoprovinces, 194ecoregions, and 1,027ecodistricts.[10] These eco-areas encompass over 80,000 classified species ofCanadian wildlife, with an equal number yet to be formally recognized or discovered.[55] Due to pollution,loss of biodiversity, over-exploitation of commercial species, invasive species, and habitat loss, there are currently more than800 wild life species at risk of being lost.[56]

Canada's major biomes are thetundra,boreal forest,grassland, andtemperate deciduous forest.British Columbia contains several smaller biomes, including;mountain forest which extends toAlberta, and a smalltemperate rainforest along thePacific coast, thesemi arid desert located in theOkanagan andalpine tundra in the higher mountainous regions.[57]

Over half of Canada's landscape is intact and relatively free of human development.[58] Approximately half of Canada is covered by forest, totaling around 2.4 million km2 (0.93 million sq mi).[59] Theboreal forest of Canada is considered to be the largestintact forest on Earth, with around 300,000 square kilometres (120,000 sq mi) undisturbed by roads, cities or industry.[60] TheCanadian Arctic tundra is the second-largest vegetation region in the country consisting of dwarfshrubs,sedges andgrasses,mosses andlichens.[61]

Approximately 12.1 percent of the nation's landmass and freshwater areconservation areas, including 11.4 percent designated asprotected areas.[18] Approximately 13.8 percent of its territorial waters are conserved, including 8.9 percent designated as protected areas.[18]

Palaeogeography

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Mount Edziza, astratovolcano in northwestern British Columbia
 
A topographic map of Canada, showing elevations shaded from green (lower) to brown (higher)

Volcanic activity is a major part of thegeology of Canada and is characterized by many types of volcaniclandform, includinglava flows,volcanic plateaus,lava domes,cinder cones,stratovolcanoes,shield volcanoes,submarine volcanoes,calderas,diatremes, andmaars, along with less common volcanic forms such astuyas andsubglacial mounds.

ThoughCanada's volcanic history dates back to thePrecambrian eon, at least 3.11 billion years ago, when its part of theNorth American continent began to form,[62] volcanism continues to occur inWestern andNorthern Canada in modern times, where it forms part of an encircling chain of volcanoes and frequentearthquakes around thePacific Ocean called thePacific Ring of Fire.[63] Because volcanoes in Western and Northern Canada are in relatively remote and sparsely populated areas and their activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Ring of Fire between the volcanoes of thewestern United States to the south and theAleutian volcanoes ofAlaska to the north.[64] Even so, the mountainous landscapes of the Canadian provinces ofAlberta,British Columbia,Yukon, and theNorthwest Territories include more than 100 volcanoes that have been active during the past two million years and whose eruptions have claimed many lives.[64]

Volcanic activity is responsible for many of Canada's geological and geographical features andmineralization, including the nucleus of the North American continent, known as theCanadian Shield. Volcanism has led to the formation of hundreds of volcanic areas and extensive lava formations across Canada. The country's different volcano and lava types originate from differenttectonic settings andtypes of volcanic eruptions, ranging from passivelava eruptions to violentexplosive eruptions. Canada has a rich record of very large volumes of magmatic rock calledlarge igneous provinces, represented by deep-levelplumbing systems consisting of giantdike swarms,sill provinces and layeredintrusions.[65] The most capable large igneous provinces in Canada areArcheangreenstone belts estimated at 3.8 to 2.5 billion years old, containing a rare volcanic rock calledkomatiite.[65]

Hydrography

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Rivers of Canada

Canada holds vast reserves of water: its rivers discharge nearly 7% of the world's renewable water supply,[66]Canada has over 2,000,000 lakes—563 greater than 100 square kilometres (39 sq mi)—which is more than any other country and has the third largest amount ofglacier water.[67] Canada is also home to about twenty five percent (134.6 million ha) of the world'swetlands that support a vast array of local ecosystems.[68]

Canada's waterways host forty-seven rivers of at least 600 kilometres (370 mi) in length, with the two longest being theMackenzie River, that begins atGreat Slave Lake and ends in theArctic Ocean, with its drainage basin covering a large part of northwestern Canada, and theSaint Lawrence River, which drains theGreat Lakes into theGulf of St. Lawrence ending in theAtlantic Ocean. The Mackenzie, including its tributaries is over 4,200 kilometres (2,600 mi) in length and lies within the second largestdrainage basin of North America, while the St. Lawrence 3,058 kilometres (1,900 mi) in length, drains the world'slargest system of freshwater lakes.[69]

The Atlantic watershed drains the entirety of theAtlantic provinces (parts of the Quebec-Labrador border are fixed at the Atlantic Ocean-Arctic Oceancontinental divide), most of inhabited Quebec and large parts of southern Ontario. It is mostly drained by the economically important St. Lawrence River and its tributaries, notably theSaguenay,Manicouagan, and Ottawa rivers. The Great Lakes andLake Nipigon are also drained by the St. Lawrence. TheChurchill River andSaint John River are other important elements of the Atlantic watershed in Canada.[70]

 
Drainage basins of Canada

TheHudson Bay watershed drains over a third of Canada. It covers Manitoba, northern Ontario and Quebec, most of Saskatchewan, southern Alberta, southwestern Nunavut, and the southern half ofBaffin Island. This basin is most important in fighting drought in theprairies and producing hydroelectricity, especially in Manitoba, northern Ontario and Quebec. Major elements of this watershed includeLake Winnipeg, Nelson River, the North Saskatchewan andSouth Saskatchewan Rivers,Assiniboine River, andNettilling Lake on Baffin Island.Wollaston Lake lies on the boundary between the Hudson Bay and Arctic Ocean watersheds anddrains into both. It is the largest lake in the world that naturally drains in two directions.[70]

Thecontinental divide in the Rockies separates the Pacific watershed in British Columbia and Yukon from the Arctic and Hudson Bay watersheds. This watershed irrigates the agriculturally important areas of inner British Columbia (such as theOkanagan andKootenay valleys), and is used to produce hydroelectricity. Major elements are the Yukon,Columbia and Fraser rivers.[70]

The northern parts of Alberta, Manitoba, and British Columbia, most of Northwest Territories and Nunavut, and parts of Yukon are drained by the Arctic watershed. This watershed has been little used for hydroelectricity, with the exception of the Mackenzie River. ThePeace, Athabasca andLiard Rivers, as well as Great Bear Lake and Great Slave Lake (respectively the largest and second largest lakes wholly enclosed by Canada) are significant elements of the Arctic watershed. Each of these elements eventually merges with the Mackenzie, thereby draining the vast majority of the Arctic watershed.[70]

The southernmost part of Alberta drains into the Gulf of Mexico through theMilk River and its tributaries. The Milk River originates in the Rocky Mountains ofMontana, then flows into Alberta, then returns into the United States, where it is drained by theMissouri River. A small area of southwestern Saskatchewan is drained byBattle Creek, which empties into the Milk River.[70]

Natural resources

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Canada's abundance ofnatural resources is reflected in their continued importance in theeconomy of Canada. Major resource-based industries arefisheries,forestry, agriculture,petroleum products and mining.[71]

The fisheries industry has historically been one of Canada's strongest. Unmatchedcod stocks on theGrand Banks of Newfoundland launched this industry in the 16th century. Today these stocks are nearly depleted, and their conservation has become a preoccupation of theAtlantic Provinces. On the West Coast,tuna stocks are now restricted. The less depleted (but still greatly diminished)salmon population continues to drive a strong fisheries industry. Canada claims 22 km (12 nmi) of territorial sea, a contiguous zone of 44 km (24 nmi), anexclusive economic zone of 5,599,077 km2 (2,161,816 sq mi) with 370 km (200 nmi) and a continental shelf of 370 km (200 nmi) or to the edge of the continental margin.

Five per cent of Canada's land area is arable, none of which is for permanent crops. Three per cent of Canada's land area is covered by permanent pastures. Canada has 7,200 square kilometres (2,800 sq mi) of irrigated land (1993 estimate). Agricultural regions in Canada include the Canadian Prairies, theLower Mainland and various regions within theInterior of British Columbia, theSt. Lawrence Basin and the CanadianMaritimes. Main crops in Canada includeflax,oats, wheat, maize,barley,sugar beets andrye in the prairies; flax and maize inWestern Ontario; Oats and potatoes in the Maritimes.Fruit and vegetables are grown primarily in theAnnapolis Valley of Nova Scotia,Southwestern Ontario, theGolden Horseshoe region of Ontario, along the south coast ofGeorgian Bay and in theOkanagan Valley of British Columbia. Cattle andsheep are raised in the valleys and plateaus of British Columbia. Cattle, sheep andhogs are raised on the prairies, cattle and hogs in Western Ontario, sheep and hogs in Quebec, and sheep in the Maritimes. There are significant dairy regions in central Nova Scotia, southern New Brunswick, the St. Lawrence Valley,northeastern Ontario, southwestern Ontario, theRed River valley of Manitoba and the valleys in theBritish Columbia Interior, onVancouver Island and in theLower Mainland.

 
The bulk of oil and gas production occurs in theWestern Canadian Sedimentary Basin (mostly light green), which stretches from southwesternManitoba to northeasternBritish Columbia.

Fossil fuels are a more recently developed resource in Canada, withoil andgas being extracted from deposits in theWestern Canadian Sedimentary Basin since the mid-1900s. While Canada'scrude oil deposits are fewer, technological developments in recent decades have opened up oil production in Alberta'sOil Sands to the point where Canada now has some of the largest reserves of oil in the world. In other forms, Canadian industry has a long history of extracting large coal and natural gas reserves.

Canada's mineral resources are diverse and extensive. Across the Canadian Shield and in the north there are large iron,nickel,zinc, copper, gold, lead,molybdenum, anduranium reserves. Large diamond concentrations have been recently developed in the Arctic, making Canada one of the world's largest producers. Throughout the Shield there are many mining towns extracting these minerals. The largest, and best known, isSudbury, Ontario. Sudbury is an exception to the normal process of forming minerals in the Shield since there is significant evidence that theSudbury Basin is an ancientmeteoriteimpact crater. The nearby, but less knownTemagami Magnetic Anomaly has striking similarities to the Sudbury Basin. Its magnetic anomalies are very similar to the Sudbury Basin, and so it could be a second metal-rich impact crater.[72] The Shield is also covered by vast boreal forests that support an important logging industry.

Canada's many rivers have afforded extensive development of hydroelectric power. Extensively developed in British Columbia, Ontario, Quebec and Labrador, the many dams have long provided a clean, dependable source of energy.

Environmental issues

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Industry is a significant source of air pollution in Canada.

Air pollution and resultingacid rain severely affects lakes and damages forests.[54] Metal smelting, coal-burning utilities, and vehicle emissions impact agricultural and forest productivity. Ocean waters are also becoming contaminated by agricultural, industrial, mining, and forestry activities.[54]

Globalclimate change and the warming of the polar region will likely cause significant changes to the environment, including loss of thepolar bear,[73] the exploration for resource then the extraction of these resources and an alternative transport route to thePanama Canal through theNorthwest Passage.

Canada is currently warming at twice the global average, and this is effectively irreversible.[74]

Political geography

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For historical political boundaries of Canada, seeTerritorial evolution of Canada.
 
A political map of Canada showing its 10 provinces and 3 territories

Canada is divided intoten provinces and three territories. According toStatistics Canada, 72.0 percent of the population is concentrated within 150 kilometres (93 mi) of the nation's southern border with the United States, 70.0% live south of the49th parallel, and over 60 percent of the population lives along the Great Lakes and St. Lawrence River betweenWindsor, Ontario, andQuebec City. This leaves the vast majority of Canada's territory as sparsely populated wilderness; Canada's population density is 3.5 people per square kilometre (9.1 people/sq mi), among the lowest in the world. Despite this, 79.7 percent of Canada's population resides in urban areas, where population densities are increasing.[75]

Canada shares with the U.S. the world'slongest binational border at 8,893 kilometres (5,526 mi); 2,477 kilometres (1,539 mi) are withAlaska. The Danish island dependency ofGreenland lies to Canada's northeast, separated from theCanadian Arctic islands byBaffin Bay andDavis Strait. As of June 14, 2022, Canada shares a land border with Greenland on Hans Island.[76] The French islands ofSaint Pierre and Miquelon lie off the southern coast ofNewfoundland in theGulf of St. Lawrence and have a maritime territorial enclave within Canada'sexclusive economic zone.[77]

Canada's geographic proximity to the United States has historically bound the two countries together in the political world as well. Canada's position between theSoviet Union (now Russia) and the U.S. was strategically important during theCold War since the route over the North Pole and Canada was the fastest route by air between the two countries and the most direct route forintercontinental ballistic missiles. Since the end of the Cold War, there has been growing speculation thatCanada's Arctic maritime claims may become increasingly important ifglobal warming melts the ice enough to open theNorthwest Passage.

See also

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Geography by province

References

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Further reading

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External links

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