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    In New France, 80 per cent of the population lived in rural areas governed by this system of land distribution and occupation. The seigneurial system was an institutional form of land distribution established in New France in and officially abolished in In New France80 per cent of the population lived in rural areas governed by this system of land distribution and occupation.

    In principle, the seigneur granted a piece of land to a family under a royalty system. The family would engage in subsistence farming to meet most of their food, heating, and shelter needs. The seigneurial system was based on the feudal system, which involved the personal dependency of censitaires tenants on the seigneur. In New France the similarities ended with occupation of land and payment of certain dues. The tenant was normally referred to as a habitant. The land was therefore granted as fiefs and seigneuries to the most influential colonists who, in turn, granted tenancies.

    Systematic Settlement This politically determined system of land distribution was regulated by law and had many advantages. Its purpose was to promote settlement in a systematic way. Seigneuries, which were usually 1 x 3 leagues 5 x 15 km in size, were generally divided into river lots rangsa survey system based on the French experience in Normandy. The long, rectangular strips were particularly well adapted to the local terrain, since they facilitated interaction between neighbours and provided multiple points of access to the river, the principal communication route.

    Individual holdings were large enough usually about 3 x 30 arpents to provide a reasonable living to farmers. The state established regulations to govern the system and the relationship between seigneurs and their tenants.

    The principal regulation granted a person, who thus became seigneur, a parcel of land that was to put into production, either directly or through concession to habitants who requested land. Portions of the seigneur's land were usually leased on the basis of a duly notarized contract. These acts of concession set out the rights and obligations of each party.

    The seigneur had both onerous and honorary rights.

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    He could establish a court of law, operate a mill and organize a commune. He received from the habitants various forms of rent: He also usually granted hunting, fishing and woodcutting licences.

    Social Hierarchy and Inequality The seigneurial system is often presented as a basic form of land distribution and occupation. However, recent studies have called for a re-evaluation of this traditional interpretation and have highlighted an aspect of the seigneurial system that is often neglected.

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    As an institution, the seigneurial system played a leading role in building and maintaining social relations in New France. However, this is not to suggest that the seigneuroppressed the censitaire. The availability of land in the 17th and 18th centuries allowed habitants to choose where to settle. Furthermore, seigneurswho were too demanding, who were absentee landowners, or who neglected to develop their lands were less likely to attract settlers. Despite the attractions of city life and the fur trade, 75 to 80 per cent of the population lived on seigneurial land until the midth century.

    Roughly seigneuries were granted during the French regime. Seigneuries were granted to the nobility, to religious institutions in return for education and hospital servicesto military officers and to civil administrators. Other institutional organizations such as parishes, municipalities and the militia held land bordering on these seigneuries. The land of the habitant was a kind of economic unit essential for survival. Everyone hoped to be the sole tenant, producing most of what he required in order to live.

    The system of land tenure, which placed rural inhabitants close to one another, and in the early 19th century the village, were the foundation upon which the family, neighbour relations and community spirit developed. The closeness of this agricultural society to the soil led naturally to a feeling that land was included in one's patrimony, to be passed from generation to generation. Development of Town System After Canada was ceded to Britain in see Treaty of Parisnew British laws respected the private agreements and the property rights of francophone society, and the seigneurial system was maintained.

    But as new land was opened for colonization, the township system developed. As time went on, the seigneurial system increasingly appeared to favour the privileged and to hinder economic development.

    After much political agitation, it was abolished in by a law that permitted tenants to claim rights to their land. Every year on St. While the Seigniorial Act of abolished the system of rights and obligations, neither seigneurial property nor the relationship between seigneurand censitairewas abolished. The amount received was then transferred to the SNRRS to be used to repay the loan over a year period. In short, the impact and importance of the seigneurial system goes beyond landscape and toponymy see Place names.

    Some former seigneurs played central roles in municipal politics and became the first mayors of their localities. For example, in the 20th century, several seigneurial honours were bestowed on descendants of seigneurial families, including Pierre Boucher of Bouchervillewho was interred beneath the Sainte-Famille church in Boucherville in Perceptions of the Tessier family of Beauport and the Taschereau family of Sainte-Marie de Beauce are influenced by their ties to the seigneurial system.
    Geographical extent[ edit ] The Canadian Shield is a physiographic divisionconsisting of five smaller, physiographic provinces: The Canadian Shield is U-shaped and is a subsection of the Laurentia craton signifying the area of greatest glacial impact scraping down to bare rock creating the thin soils.

    The Canadian Shield is more than 3. The Canadian Shield once had jagged peaks, higher than any of today's mountains, but millions of years of erosion have changed these mountains to rolling hills. It is the Earth's greatest area of exposed Archean rock. The metamorphic base rocks are mostly from the Precambrian Supereon between 4.

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    During the Pleistocene Epoch, continental ice sheets depressed the land surface see Hudson Bayscooped out thousands of lake basins, and carried away much of the region's soil. When the Greenland section is included, the Shield is approximately circular, bounded on the northeast by the northeast edge of Greenland, with Hudson Bay in the middle.

    It covers much of Greenland, Labradormost of Quebec north of the St. The true extent of the Shield is greater still and stretches from the Western Cordillera in the west to the Appalachians in the east and as far south as Texas, but these regions are overlaid with much younger rocks and sediment. The underlying rock structure also includes Hudson Bay.

    Canadian Shield geography in the Flin FlonManitoba region. The lake in the background is Big Island Lake. Weathered Precambrian pillow lava in the Temagami Greenstone Belt The Canadian Shield is among the oldest on earth, with regions dating from 2.

    The Shield was originally an area of very large, very tall mountains about 12, metres or 39, feet [10] with much volcanic activity, but over hundreds of millions of years, the area has been eroded to its current topographic appearance of relatively low relief. Many of Canada's major ore deposits are associated with Precambrian volcanoes.

    The Sturgeon Lake Caldera in Kenora District, Ontariois one of the world's best preserved mineralized Neoarchean caldera complexes, which is 2. Mountains have deep roots and float on the denser mantle much like an iceberg at sea.

    As mountains erode, their roots rise and are eroded in turn. The rocks that now form the surface of the Shield were once far below the Earth's surface. The high pressures and temperatures at those depths provided ideal conditions for mineralization. Although these mountains are now heavily eroded, many large mountains still exist in Canada's far north called the Arctic Cordillera.

    This is a vast deeply dissected mountain rangestretching from northernmost Ellesmere Island to the northernmost tip of Labrador. The North American craton is the bedrock forming the heart of the North American continent and the Canadian Shield is the largest exposed part of the craton's bedrock. The Canadian Shield is part of an ancient continent called Arcticawhich was formed about 2.

    Ecology[ edit ] The current surface expression of the Shield is one of very thin soil lying on top of the bedrockwith many bare outcrops. This arrangement was caused by severe glaciation during the ice agewhich covered the Shield and scraped the rock clean. The lowlands of the Canadian Shield have a very dense soil that is not suitable for forestation; it also contains many marshes and bogs muskegs.

    The rest of the region has coarse soil that does not retain moisture well and is frozen with permafrost throughout the year. Forests are not as dense in the north. Typical landscape in a southern Ontario region with very few old growth trees, due to a history of logging and fires. The Shield is covered in parts by vast boreal forests in the south that support natural ecosystems as well as a major logging industry. This boreal forest area includes ecoregions such as the Eastern Canadian Shield taiga that covers northern Quebec and most of Labrador, and the Midwestern Canadian Shield forests that run westwards from Northwestern Ontario.

    Hydrographical drainage is generally poor, the soil compacting effects of glaciation being one of the many causes.

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    Tundra typically prevails in the northern regions. Many mammals such as caribouwhite-tailed deermoosewolveswolverinesweaselsminkottersgrizzly bearpolar bears and black bears are present. It is filled with substantial deposits of nickelgoldsilverand copper. Throughout the Shield there are many mining towns extracting these minerals.

    The largest, and one of the best known, is SudburyOntario. Sudbury is an exception to the normal process of forming minerals in the Shield since the Sudbury Basin is an ancient meteorite impact crater.

    Ejecta from the meteorite impact was found in the Rove Formation in May The nearby, but less known Temagami Magnetic Anomalyhas striking similarities to the Sudbury Basin. This suggests it could be a second metal-rich impact crater. This is one of the largest-known meteorite impact craters on Earth.

    The Flin Flon greenstone belt in central Manitoba and east-central Saskatchewan is one of the largest Paleoproterozoic volcanic-hosted massive sulfide VMS districts in the world, containing 27 copper - zinc - gold deposits from which more than million tons[ clarification needed ] of sulfide have been mined. The kimberlite pipes in which the diamonds are found are closely associated with cratons, which provide the deep lithospheric mantle required to stabilize diamond as a mineral.

    Currently the Ekati and Diavik mines are actively mining kimberlite diamonds.

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