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The 'Geography of Manitoba' is the easternmost of the three prairie provinces, and is located in the longitudinal center of Canada. It borders on Saskatchewan to the west, Ontario to the east, Nunavut to the north, and the American states of North Dakota and Minnesota to the south. On comparative level, Manitoba ranges from 490 ft (150 m) to 980 ft (300 m) above sea level.^[1] Baldy Mountain, which is its highest point, is at 2727 ft (831 m). The northern 3/5 of the province is on the Canadian Shield. The northernmost regions of Manitoba lie in tundra and permafrost (permanently frozen subsoil).
All waters in the province flow into Hudson Bay, due to its coastal area. Lake Winnipegosis and Lake Winnipeg are two of its largest lakes. Important rivers are the Red River, Assiniboine River, Nelson River, and Churchill River.
Manitoba has an extreme climate, but southern latitudes allow extensive growth for agriculture. The northern area of the region ranges from coniferous forests to muskeg to tundra in the far north. Before settlement had occurred, a vast portion of southern Manitoba was either flood plain or swamp.^[2]. An extensive system for drainage ditches was required for construction throughout south central Manitoba to make the region suitable for cultivation.

Contents

Historical geography

Mountain ranges of Manitoba

Landscape past and present

Other facts

Miscellaneous

Area

Population

References

Notes

See also

External links

Historical geography

It is bordered on the east by Ontario, and south by North Dakota and Minnesota, on the west by Saskatchewan, and north to Nunavut. Northeast Manitoba follows the Hudson Bay shoreline. Churchill, on the Hudson Bay is the only port for itself and the remaining prairie provinces. The harbour serves as an open market for grain.
Manitoba was the first province to be involved in the wheat industry. There are only three ice-free months a year that allow for the shipments to be sent.
The Canadian Shield limits the amount of farming in the north, but there are some forestry and mining operations. The majority of the grain production is found in farms in the south.
Central and southern Manitoba is covered by lakes and rivers. Most of the population is centered in the southern third of the province.^[3]
Manitoba played a significant role in the population of the Canadian west. Explores arrived in Manitoba by the Hudson Bay, in search of a passage to China. As the fur trade boomed, settlements rose up in the province to trading posts for the Natives and the Voyageurs (trappers). The settlement was not easy, and colonization slowed down for several years (1816). In 1870, the Hudson's Bay Company sold its huge domain to the confederation of Canada.
Settlement inflated in Manitoba when the railway was built in the province and again in late 18th, early 19th century when government promoted settlement by European immigrants.

Mountain ranges of Manitoba

The three dominant mountain ranges in Manitoba consist of Duck Mountain, the Pembina Mountains, and the Porcupine Mountains. They encompass natural beauty, tourist attractions, resorts, provincial parks, and many recreational activities.
The Duck mountain range is located in western Manitoba and stretches along the north-south Saskatchewan border. The highest point is Baldy Mountain, which reaches 2, 727 feet. Duck Mountain Provincial park is located within the range and includes vivid scenery, tranquil Madge Lake, aspen forests, beaches, campgrounds, and fishing.^[4]
The Pembina Mountains are located in southern Manitoba and extends over to Assiniboine River and the North Dakota border. Its highest point is 2, 000 feet.
The Porcupine Mountains range is located in west-central Manitoba and extending along the Saskatchewan border. The highest point, which is Hart Mountain near Swan River, rises to 2,700 feet. The area is for divers habitats, ranging from prairies to glacier valleys to plateaus and well-known for its dense forest.

Landscape past and present

Early activity in the region, which would eventually become the Strathclair district, was centered on the Little Saskatchewan River and its valley which is about midway between Riding Mountain and the Assiniboine River. The river, a meandering tributary of the Assiniboine, flows south from Lake Audy and Clear Lake, both situated in present day Riding Mountain National Park. It then follows a generally southeastward course through a fertile, deep, and diverse valley. Members of at least two early exploratory expeditions, those led by Dickinson and Hind, recognized the valley as one of the best in the northwest in terms of settlement potential.^[5] The deep alluvial soil was accompanied by an abundance of good water, pasture, and forests. It also provided a relatively easy transportation route for water cargo. It is the location of where the river turns southeast (sec. 36 twp. 17 rge. 22 WPM) that the first settlement took place. The location also gives the settlement its name, the Bend.
The area of the North Bend was marked with sloughs and lakes interspersed with stands of poplar, spruce, and birch. It eventually became the Riding Mountain Timber Reserve (and then RMNP) and the Keeseekoowenin Indian Reserve. With skilled hunting, trapping, and fishing there was raised for the Hudson Bay's company Trading post upstream near the present site of Elphinstone. The rolling hills and hills of the south of the bend starked contrast to woodland in the north. Unobstructed prevailing western westerlies fanned prairie fires in the summer and whipped up blizzards in the winter. Indian tribes for a while encouraged fire to enhance grassland for buffalo grazing and an early settler, Lord Elphinstone, found out that the grazing grounds lent themselves to thriving ranching enterprises. Wood for fuel and buildings were hauled from the river valley or from farther north, though immediately as the land was broken, bluffs of poplars took root and spread out from the low-lying potholes or sloughs.
Several settlement sprung up before the railway was made. Farther East were the Forks (33-15-21) at Carlton Trail continued on its western route to Fort Ellice in the upper Assiniboine while a branch broken northward to The Bend. It followed Lake Audy, continued to the Gilbert Plains, Great Daulphins, and Swan river valley. Many settlers traveling north took Strathclair-Dauphin Colonization Trail to find the firmest ground, and easiest camping.
The Bend, Riding Mountain HBC Post, Old Marney and The Forks were joined by the river, cart routes and Indian trails. By the mid seventies, a section town range grid was placed in for future house settlements. Waggon loads of adventurous Scots from the east began to arrive on rail to Winnipeg. The Bend was renamed Strathclair, a portmanteau of the Scottish word "strath" for valley and "clair" from the surveyor his name; it then came the Manitoba and North Western Railway (now a branch of the Canadian Pacific Railway), traversed the area midway between The Bend (Old Strathclair) and Old Marney. Before the end of the century, the for settlements had evolved into another location.
The event had a major effect on the development of Manitoba. It was modified to the technological and cultural changes bought by railway. In addition, the railroad company held the rights to the land in the direction, the town's mark stretched along the northeast side of the main street, that ran the parallel to the tracks in northwest-southeast direction, characteristic to many other prairie towns.
The land companies brought on extensive advertising campaigns to persuade new settlers, resulting in a flood of newcomers, and infusion into the area of a much more diverse ethnic mixture. In 1888, the Premier of Manitoba, John Norquay, had a summer in the north east coast of Salt Lake, a current popular picnic and resort spot. He had planned to erect the sanatorium there, when immediately he died, turning the century, Stratclair became a firm and successful farming society.

Other facts

===Location and Boundary===

★ Area: 250,946 miles / 649,950 km

★ Land Surface: 211,721 miles / 548,360 km

★ North to South: 761miles / 1225 km

★ Width (South): 279 miles / 449 km

★ North Boundary (Width): 260 miles / 418 km

★ Coastline: 400 miles / 645 km

★ ''Water surface'': 39,225 miles / 101,593km

★ Widest Point: 493 miles / 793 km

Miscellaneous

★ Capital: Winnipeg

★ Largest City: Winnipeg

Area

★ Total

★ 8th largest % of fresh water

★ The 6th largest province

Population

★ Total (2001): Density Ranked 5th

★ 1 150 000

★ 1.78/km²
Time zone UTC: -6

References

Notes

★ Manitoba Geography

★ Manitoba

★ Manitoba historical geography

★ Mountain ranges

★ Praire:Manitoba: Strathclair by John Welsted, John Everitt and Christoph Stadel of University of Manitoba Press

See also

★ Geography of Canada

★ List of highest points of Canadian provinces and territories

External links

★ Manitoba Provincial Unit Study

★ Manitoba Geology

★ Answers.com for Manitoba