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INTERIOR PLAINS PHOTOS INTERIOR PLAINS PHOTOGRAPHIC REVIEW



Southern Manitoba

Contact zone between the Canadian Shield and the Interior Plains southeast of Winnipeg. The Interior Plains area is dominated by Mesozoic sedimentary rock. After the last glacial period, clays, silts and sands were laid over the sedimentary bedrock. Lacustine plains (clayey lake deposits), kame deltas (sandy deposits), morainic features (coarser textured materials), meltwater channels (broad river valleys) and erratics (large boulders) are some of the features associated with wastage of the last large ice sheet that once covered this region. These glacial deposits and soils that developed over them during the last 10,000 years, provide a good base for domesticated plant production (e.g., wheat, barley, canola, etc.). The flat plains area (lacustrine plain) has been intensively developed as farmland; the transition zone between the plains and the shield area has scattered farmlands, and the shield proper is not suited to agricultural production due to poor soil and/or drainage conditions. Winters in this area tend to be cold and dry. Summers are generally mild, however, intensive convection can produce violent thunderstorms and heavy rainfall. Hot, humid air from the Gulf of Mexico can penetrate this far north during July and August. The Manitoba Plain (extending from the Shield in the east to the Manitoba Escarpment in the west) was the first to be colonized in the Interior Plains. What group first settled in this area?
Photographer : J. Lewis Robinson
Perspective:
Date:
Reference: pr-2


Winnipeg

Winnipeg is sited at the confluence of the Red and Assiniboine Rivers. In 1733 the La Verendrye brothers, a French fur traders based out of Montreal, establish a fur-trading post at this site. The Montreal-based traders were to establish a number of posts along the North and South Saskatchewan Rivers. Trade in beaver pelts was the primary activity. The Hudson's Bay Company had been granted a charter by Charless II of England to trade among the natives living in the Hudson's Bay drainage basin. For nearly 100 years the HBC operated posts along the western edge of the Hudson's Bay; however, as the French traders moved into the Red River valley and the Saskatchewan watershed, the HBC quickly established inland posts. Intense competition for furs ensued between the HBC and the major Montreal company -- the North West Company. Intense competition for furs (mostly beaver pelts used to make felt hats) found expression across the western interior. This rivalry ended in 1821 when the North West Company was amalgamated with the Hudson's Bay Company. HBC was to build a new headquarters at Lower Fort Gary, located downstream from Winnipeg (Upper Fort Garry). For more on the early history of Winnipeg and the fur trade you may wish to consult Winnipeg -- Our Colourful Past
Photographer : D. Stone
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Reference: pr-3


Lower Fort Garry

Located near Selkirk, Lower Fort Garry was built by the HBC on a high bluff overlooking the Red River. This became the new headquarters for the HBC. Sturdy stone buildings were constructed to store furs that were gathered from the various trading posts scattered throughout the interior. From here, bundles of furs would continue their voyage via canoe brigade to Montreal. Red River carts were introduced by the Metis (mixed-blood -- usually French-Indian) who continued the native practice of hunting bison on the open prairies to the west of the Red River. Buffalo meat and furs would be returned to Upper and Lower Fort Garry for domestic use. Dried buffalo meat (pemmican) became a staple food among the early fur-traders. It was light and nutritous and could be transported easily.
Photographer : D. Stone
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Reference: pr-7


Red River Valley

Early French influence in the Red River valley remains in the landscape. Long lots extend outward from the Red River both north and south of Winnipeg. In 1812, Scottish crofters arrived at Fort Garry (later Upper Fort Garry) to settle. Although tolerated by the HBC, the settlers were never welcomed by the fur-traders nor the resident Metis who supplied the wilderness posts with pemmican. Poor crops brought on by inadequate moisture and insect infestation were exacerbated by a rather hostile resident population (fur-traders and Metis hunters). The Selkirk settlement failed; some hung around Fort Garry, some moved south to the U.S. and others ended up in the Maritimes.
Photographer : J. Lewis Robinson
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Reference: pr-9


Red River Valley

The long lots of the Red River valley resemble those found in the St. Lawrence River valley. However, the similarity ends here. No seigneural system was introduced to the Red River area because the French empire in North America had ended by 1763. Nonetheless, the rural settlement pattern is distinctly Quebecois. How would you described the rural settlement pattern in the photo?
Photographer: D. Stone
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Date:
Reference: pr-10


Southern Manitoba

Until 1931, the Government of Canada, under the Department of the Interior, was responsible for settling the interior plains. Once British Columbia joined Confederation in 1871 on the promise of a trans-continental railway, this opened the way for the lands lying north of the 49th parallel to be surveyed and ready for settlement. Firstly, the government needed to "make treaties" with the aboriginal peoples of the plains in order to ensure that this vast tract of territory would be available for settlement. Secondly, the government had to survey the lands quickly to ensure that they would be settled by peoples loyal to Canada. The American-styled township, section and range system was chosen as the most expedient way of surveying this enormous, largely unoccupied, territory. Using a base line on the eastern edge of the plains, a grid survey system comprising townships, sections, ranges, and quarter-sections was imposed across the plains landscape. A township was the larger unit -- comprising 36 sections or 36 square miles. Each section (640 acres) was 1 square mile in size and was further surveyed into quarter-sections (160 acres). The quarter-section, 1/4 square mile or 160 acres, became the basic areal unit for homesteading, leasing or land purchase. Under the Homestead Act, the federal government was responsible for disposing of Crown (public) lands throughout the interior plains. As part of the Canadian Pacific Railway Company's compensation from government for constructing a trans-continental railway from Montreal to the west coast was the delivery to the railway company of large tracts of quarter-sections; likewise, once the HBC relinquished its monopolistic control of commerce in the western territory, it too received land grants from the federal government. Two sections in each township was reserved as School Lands -- a measure to support the early public education system in the Canadian west.
Photographer: D. Stone
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Reference: pr-11


Rhineland

The first large-scale immigration of agricultural settlers into the plains region were the Mennonites from central Europe. The Government of Canada allowed the Mennonites to retain their traditional lifestyle. Evidence of this remains in the rural landscape of southern Manitoba (e.g., the Altona area). Nucleated rural villages, such as Rhineland, were allowed to develop. Farmers from the village would cultivate individually-owned 1/4 sections beyond the village. Later settlers to the prairies and parkland regions were required to settle on individual 1/4 sections. Once specified homestead duties ("x" number of acres placed under cultivation, "x" number of livestock, built a habitable home, etc.) had been fulfilled, the homesteader received patent (ownership) from the Crown (government) to the land. What would these rural villagers grow on their individual plots of land behind their farm buildings?
Photographer: J. Lewis Robinson
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Reference: pr-12


Southern Manitoba

The idea of the connected house and barn was introduced into the Manitoba landscape by the early Mennonite settlers. The design of these structures was simple; the scale rather large. Each farmstead had barns, sheds, granaries (later silos), corrals, pigsties, chicken coops, and gardens (foreground). Early settlers brought valued vegetable seeds from their native lands.
Photographer: D. Stone
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Date:
Reference: pr-14


Southeastern Manitoba

Ukranian settlers were another large ethnic group (i.e., non Anglo) who settled in southern Manitoba. They settled some of the poorer lands to the east of the Mennonite settlements. Arriving later, much of the good land had already been settled. Like the Mennonites, they brought with them their cultural traditions, including how to construct a house. Hewn logs and plaster were commom building materials. Roofs were originally made of thatch; later shingles.
Photographer: J. Lehr
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Reference: pr-15


Southeastern Manitoba

In addition to settling in southeastern Manitoba, large Ukranian settlements were to emerge in the parkland belt, notably at Dauphin (Manitoba) Yorkton (Saskatchewan) and Vegreville (Alberta). Ukranian settlers tended to be either adherents to the Eastern Christian Church (Greek Orthodox -- patriach in Istanbul, formerly Constantinople) or to the Western Christian Church (Greek Catholic -- pope in Rome). This Greek Catholic church once provided the focal point for religous and social gatherings in the early settlement period.
Photographer : D. Stone
Perspective: Looking southeast
Date: Spring, 1978
Reference: pr-16


Hecla Provincial Park

Nearly 100 years ago, Icelanders moved into the Interlake (region located between Lake Winnipeg and Lake Manitoba) to engage in fishing and farming. The land here could be either stoney or poorly drained. Spring and fall frosts were a hazard for crop production. Many of the poorer areas were abandoned. Today, this small community is located in Hecla Provincial Park, noted for its fine golf course along the shores of Lake Winnipeg.
Photographer: D. Stone
Perspective: Looking north
Date:
Reference: pr-62


Winnipeg

Sugar beet production by farmers in southern Manitoba supports this sugar beet refinery on the southern outskirts of Winnipeg. White sugar can be refined from sugar beets; cane sugar from tropical regions is used to produce brown sugar.
Photographer: D. Stone
Perspective: Looking south
Date:
Reference: pr-55


Spruce Woods Provincial Park

With the retreat of the last continental glaciers, large volumes of silts and sands were laid down as deltas at the edge of the ablating (wasting) ice sheet and an impounded lake. When the ice sheet melted and the lakes were drained, these deltas appeared as elevated features in the landscape. Winds that swept across the exposed landscape reworked these deltaic formations into sand dunes. At this location in southwestern Manitoba, the sand dune formations lie within a provincial park. Similar areas are often used as military bases (e.g., Shilo, Manitoba; Wainwright, Alberta). Ranchers may graze livestock in these areas, however, the carrying capacity is very low (i.e., the number of cattle that can be support per areal unit of land).
Photographer: D. Stone
Perspective: Looking west
Date:
Reference: pr-66


Churchill

Churchill is located on an estuary of the Churchill River that flows into Hudson Bay in northern Manitoba. Founded by the Hudson's Bay Company, this site was an important fur transshipment depot. This function was to be extended to the handling of grain with the completion of a rail line to this site in the early 1920s. The large grain terminals and handling facilities (upper foreground of photo) provided an alternative to shipping prairie grain through the Lakehead. The overall distance to ship grain from the prairies to Britain was much shorter through the Port of Churchill, however, this port is only operational for two to three months annually. Oil storage facilities are also found here. This community numbers about 800 over the winter; swells to 1500 during the summer. Tourists arrive in Churchill via rail and air. Beluga whale watching is a popular activity in the area.
Photographer: J. Lewis Robinson
Perspective: Looking south
Date:
Reference: pr-70