Preview

Canada S 7 Largest Landform Regions

Good Essays
Open Document
Open Document
350 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Canada S 7 Largest Landform Regions
Canada’s 7 major Landform Areas
Precambrian Shield/ Canadian shield:
Area: -4.8 million km, almost ½ of Canada, thus the largest landform region, (actually much larger because it underlies most other regions).
-Spreads across 6 provinces, 2 territories, and the U.S.
Formation: -about 600 million years old, thus “Precambrian”.
-Igneous and metamorphic rock.
Topography: -a peneplain, almost a plain 600 metres.
-has a lakescape, many lakes.
Human Activities:-an all season vacation land.
-Also called “Mineral Storehouse”: many metamorphic rocks: minerals such as gold, copper, nickel, lead, zinc and iron found in Region.
-Forestry is also an important industry.
-Sparsely populated, people live near mining and forestry centres and along transportation links which tie them to the rest of Canada.
Major Cities: -Sudbury, Timmins, North Bay, Yellowknife, and Uranium City.

Low lands
Great lakes-ST. Lawrence Lowlands:
Area:-Smallest of landform regions.
-Located around the great lakes and on the banks of St. Lawrence River.
-“Nations Heartland”; reaches further south.
Formation: - ancient seas, deposited materials that harden into limestones, sandstones, and shales; these all rest on top of Precambrian Igneous rocks.
-Glacial Lake deposited materials and glacial ice deposited ground Moraine; The St. Lawrence Lowlands were an in land sea during glacial period (Champlain Sea-Fertile top soil on sea bed).
Topography: -Niagara Escarpment formed by erosion of softer rocks around the hard dolomite rock: Niagara River flows over the escarpment at Niagara falls.
-A fairly Flat Region.
-Mounteregion hills are exposed to Igneous intrusions, the outlying softer materials have eroded away, creating these hills near montreal.
Human Activities: -Excellent soils deposited under glacial lakes or melting continental glaciers, excellent for farming.
-Flat excellent for settlement.
-Largest population of all of the Landform Regions.
-Region is

You May Also Find These Documents Helpful

  • Better Essays

    3rd geo report RE WRITE 3

    • 1354 Words
    • 5 Pages

    Located within the Hudson Highlands proto-continents collided giving rise to a major crustal thickening event called the Grenville Orogeny. It is important to study it because, it provides the geologic history of that particular area. In order to study the area, one must be able to identify detailed information about identifying rock types, mineral composition and associating it with its proper metamorphic facies.…

    • 1354 Words
    • 5 Pages
    Better Essays
  • Powerful Essays

    - Glaciers: large masses of ice on land that show evidence of being in motion or of once…

    • 3535 Words
    • 15 Pages
    Powerful Essays
  • Good Essays

    Not even the native people who have occupied this ecozone throughout history have dared to start large farms there. I assume that, for a farm to survive in such a harsh climate, a farmer would have to overcome a huge financial risk. So, the reason why farms have been able to start operating in the ecozone between 1971 and 2011 is because large farming companies can afford the risks involved with using Canada's cold, undeveloped land. Smaller farms that lack resources and employees would struggle to deal with the weather conditions, let alone operate in complete isolation.…

    • 540 Words
    • 3 Pages
    Good Essays
  • Satisfactory Essays

    The Canadian Shield also known as Laurentian Plateau/ Laurentian Shield and is the geographic foundation of Canada. This region was formed about 2.5 billion years ago by a volcanic eruption. The two kinds of rock that make up this shield are igneous and metamorphic rocks. The area of this region is ‎8 000 000 km2, and provinces located here are Quebec, Ontario, Manitoba, Saskatchewan, Nunavut and Northwest territories. The climate in the southern part of the shield has long and cold winters, while the northern part gets less snow/rain per year. In this region, forest is mixed with birch trees, tamarack, spruce trees, etc. Some animals found here are moose, black beaver, wolves and foxes.…

    • 115 Words
    • 1 Page
    Satisfactory Essays
  • Good Essays

    sand and soil in place. Wheat farmers plowed the short grass prairie to create wheat farms,…

    • 474 Words
    • 1 Page
    Good Essays
  • Better Essays

    Geology 101

    • 1324 Words
    • 6 Pages

    The material on the right, the gneiss – looks quite different to the peridotite. That would suggest that we may have different minerals – and different minerals mean different environment and or/different processes. The gneiss is a metamorphosed rock – so a rock that has been transformed from its original form due to heat and or pressure. Gneiss makes up most of earths lower crust – the pressure and heat transforms sedimentary and igneous rocks.…

    • 1324 Words
    • 6 Pages
    Better Essays
  • Good Essays

    Biome Paper

    • 687 Words
    • 3 Pages

    The soil isn’t a true soilbecause of the Permafrost developed, the freeze-thaw activity, a thin active layer, and solidification. This soil is moist and thin over the permafrost; furthermore the soil has low nutrients and is also slightly acidic. The Permafrost serves as a barrier to keep animals from…

    • 687 Words
    • 3 Pages
    Good Essays
  • Powerful Essays

    The Relevancy of the Heartland - Hinterland Distinction in Canada's Economic Geography Until the early 20th century, Canada was primarily an agricultural nation. Since then it has become one of the most highly industrialized countries in the world as a direct result of the development of the ‘heartland'. To a large extent the manufacturing industries present in the heartland are supplied with raw materials produced by the agricultural, mining, forestry, and fishing sectors of the Canadian economy, a region known as the ‘hinterland'.…

    • 1167 Words
    • 5 Pages
    Powerful Essays
  • Good Essays

    The Great Lakes- St Lawrence Lowlands is the smallest yet most populated region in Canada. The topography of the region was the end result of weathering and erosion from rivers of the nearby flat-early sedimentary rock. During the Paleozoic era, glacial erosion shaped the lakes into sedimentary rock. Withdrawing glaciers washed up large portions of sands, silts, and gravels as flat plains and rolling hills. Due to the Great Lakes, the climate is humid, the lakes provide the moisture in the air. The Great Lakes- Lawrence Lowlands is close to the equator which also makes the weather humid. Although it is uncommon during the summer, there is a chance of a flood if there’s an intense rainstorm. The soil in this region is very fertile, which allows many crops to be grown. Many trees, such as deciduous and conifer, walnuts, maple, hemlock, oak, and peaches can be grown. Along with…

    • 578 Words
    • 3 Pages
    Good Essays
  • Good Essays

    Canadian Shield Geography

    • 1785 Words
    • 8 Pages

    The Canadian Shield is made up of metamorphic and igneous rock, containing some of the world's oldest rocks. It had once been a major mountain region but it is now relatively flat with rounded rock hills. In addition, hundreds of thousands of lakes existed as gouging and scrapings of ice many years ago which had left depression in the bedrock. The Canadian Shield lakes are often crystal clear due to the granite on the bottom.…

    • 1785 Words
    • 8 Pages
    Good Essays
  • Good Essays

    The Intermountain Region

    • 560 Words
    • 3 Pages

    The Intermountain Region is a region that is located in parts of Canada and America, while lying between the Rocky and Coast Mountains, the Cascades and the Sierra Nevada. The high plateaus and isolated mountains with the only deserts in the US of A are very sparsely populated (excluding major cities). In Canada, this region is consisted of the interior plateau valleys of BC and the Yukon.…

    • 560 Words
    • 3 Pages
    Good Essays
  • Good Essays

    Quebec Population

    • 255 Words
    • 2 Pages

    mining, and other types of activity. The historical movement of the population in Quebec has been from large…

    • 255 Words
    • 2 Pages
    Good Essays
  • Good Essays

    Canada is not only a nation of people, it's also an uncomparable feast of wilderness and geography. Our extensive landscape of rivers, lakes, mountains, deserts, plains, tundras, and forests offers just about anything for the…

    • 499 Words
    • 2 Pages
    Good Essays
  • Good Essays

    Joshua Tree National Park

    • 539 Words
    • 3 Pages

    Another wonderful geological phenomenon is the park’s variety of mountains and their ranges. From the Pinto mountains to the Hexie mountains, their rocks are a sight to see. You can tell by these exposed granite monoliths that immense earth forces were the cause for their shape and formation. Hills formed by rock piles made of pinkish monzogranite, also share a story of formation and geological history. These rocks are formed…

    • 539 Words
    • 3 Pages
    Good Essays
  • Good Essays

    St. John Narrative

    • 755 Words
    • 4 Pages

    Lawrence Lowlands, which I had been hoping to get to. It made me oddly happy to travel across rolling hills and plain land for a change. As I made my way through Southern Ontario I felt more confident in my ability to complete my journey. During my time in the St. Lawrence Lowlands I had the privilege of seeing some amazing natural sights, such as the occasional escarpments in the landform region. In particular, Flowerpot island was a striking sight that showed the incredible power of weathering and erosion. Additionally, the abundance of freshwater lakes and rivers I saw, such as the St. Lawrence River or the Great Lakes, demonstrated how fortunate Canada is to hold so much drinkable water. I had no trouble with crossing the landform region, as there was no difficult terrain that I struggled to…

    • 755 Words
    • 4 Pages
    Good Essays