IntroductionSaskatchewan is situated in the central Prairie between Alberta on the west and Manitoba on the east. Its neighbour on the north is the North West Territories, and on the south it borders with the United States. Saskatchewan is rectangular in shape--it is the only Canadian province none of whose borders was determined by the landform feature like river or mountain range. The province is located in the Central Standard Time and doesn't switch on Daylight Saving Time in summer. The population of Saskatchewan is around one million people with the area of 651 900 km2. Physical and Natural DescriptionGeologic History--Land Formation, Types of Rocks, and Minerals The northeastern part of Saskatchewan is a part of the Canadian Shield that was formed during Precambrian era and features some of the oldest rocks in the world.
The border that separates the Canadian Shield from the rest of the province runs across Saskatchewan from south-east to north-west. This part of the province was formed during Precambrian era and contains igneous and metamorphic rocks. From the minerals found in that part of the Shield the most abundant and the most important for Saskatchewan is the metallic mineral uranium that can be used for building the nuclear reactors or exported to the other countries. The rest of the province, except for the extreme southwest which is occupied by the Hills, is situated on the Saskatchewan Plain which is a part of the Interior Plains that are, in turn, part of the Great Plains of North America. This part was formed under water when the mountains of the Canadian Shield eroded and deposited on the bottom of the shallow seas that it was surrounded by. The process was completed during the Mesozoic era. This part is relatively flat with gently rolling hills and occasional valleys.
The most important minerals that are found in this area composed of soft and hard sedimentary rock are the non-metallic minerals like potash which is widely used as a fertilizer and some oil.Major Landform Features The major landform feature of the province is the escarpment created by erosion that separates Saskatchewan Plain from Alberta Plain and Manitoba Plain. Except for the Cypress Hills near the U.S. border, Saskatchewan lies on a plain. Its landscape is not absolutely flat-...
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...National Park which 3875 km2 in area. It's a region of aspen parkland and boreal forest. It was established as a national park in 1927. Being a preserved and protected area, the park is very rich in wildlife including elk, caribou, moose, deer, lynx, otter, and plains bison. It also features the only protected White Pelican colony in Canada.
There are 31 provincial parks and another National Park called Grassland National Park Reserve that is one of the last areas where the colonies of Black-tailed prairie dogs, rattlesnakes, pronghorn, and the Prairie Falcon are found.Personal OpinionI think that Saskatchewan is a wonderful place to visit. Northern Saskatchewan is well known for its fishing and hunting camps. Another attractions are summer rodeos. If you want to explore Canada no tour will be complete without visiting the legendary prairies, thousands of lakes, wonderful nature of Saskatchewan. Even though history of Saskatchewan is not in the scope of this essay, I have to mention that Saskatchewan is where a lot of Canadian history took place--an example is the creation of the legendary North-West Canadian Mountain Police that earned great respect and reputation for fairness.
There is also moss that is found in the region which is called Feather moss, there is also a moss called Sphagnum moss. Some flowers are: Fireweed, Rosemary, Twinflower, Wild Chives, Saxifrage and Kalmia Heath ( Sagner, B. 2010 para 1). The Canadian Shield locale of Canada has heaps of creatures. A portion of the creatures are moose, wild bears, wolves, foxes, beavers, minks, martens, wolverines, lynxes, wood bison, forest caribou, vixens, weasels and rabbits. The Canadian Shield has a wide range of sorts of untamed life that can make The Canadian Shield their home because they can sufficiently discover food, water and shelter there (Canadian Shield, 2003 para 5).
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
Quebec is the largest Canadian province, with the second largest population and economy after that of Ontario. Historically, the province of Quebec presents a unique frontier for the analysis of Anglo-French relations. It is important to note that Canadian domain as a whole was principally an extension of France until the British forces led by Jeremy Amherst took hold o Montreal in 1760. The 1763 signing of the Treaty o Paris essentially sealed this acquisition of Canada by the Great Britain. The present federal structure of Canada came into being in 1867; a structure that created the office of the Prime Minister and promised considerable autonomy to the provinces. However, the relations of the French-speaking province of Quebec
Canada's heartland is southern Ontario and Quebec stretching from Quebec City to Windsor. This heartland, occupying the Great Lakes-St. Lawrence Lowlands, coincides with several favourable physical characteristics such as fertile Class 1 and 2 soils in addition to humid continental climate for optimal agricultural conditions. However, the "hinterland regions display harsher or more limiting physical characteristics. The Cordillera, Interior Plains, Canadian Shield, and Appalachian regions yield tremendous resource wealth, but their soils,
Central Intelligence agency , "Canada ." Last modified November 12, 2013. Accessed November 27, 2013. https://www.cia.gov/library/publications/the-world-factbook/geos/ca.html.
...e-not’ province related to others” Manitoba could now have the potential to become just as industrialized and important as a province such as Ontario. The whole of Canada would benefit economically from water schemes.
The Canadian Shield is a landform region that covers almost more than half of Canada, it was formed about 3 billion years ago and was formed by volcanic eruptions. The Canadian Shield has some of the world's oldest rocks and has a lot of trees, lakes and rivers, some things the Canadian Shield provides us with is minerals, water from hydroelectric power and trees. it is a medium populated area and the population is very scattered, most of the people live in the southern area.
Dheeraj Patel Journey Around Canada 2. How do the natural characteristics of Canada influence human activity, and how might human activity influence Canada’s natural characteristics? (B1) In the Central part of Canada there are many different human activities that affect natural characteristics. In the Central part of Canada there are many interior plains landforms.
The Hudson plains are in parts of Ontario and Manitoba. Their area is about 350 000 km squared. The west edge of the Hudson Plains is around Churchill in north Manitoba, the eastern edge is around Fort Rupert, the northern edge borders Hudson Bay and James Bay and the southern edge is near Kapuskasing, Manitoba. Moosonee and Churchill are major cities in the Hudson Plains area, and lesser known cities include Attawapiskat, Fort George, Eastmain, Fort Albany, Lake River, Winisk, Fort Severn, and Shamattawa.
Algonquin Park is the oldest and most famous provincial park in Ontario and one of the largest in Canada. It stretches across 7,725 kilometers of wild and beautiful lakes and forests, bogs and rivers, cliffs and beaches. This is why Algonquin is also known as a canoeist's and camper's paradise as far as the eye can see.
The ecozone's forests are composed of 12.8% mixedwood, 2.1% deciduous, and 0.2% coniferous trees. The forest cover spans from 3 to 16%, and 40% of Ontario's rare plants are exclusive to the Carolinian forests. The Wood Poppy, Small-whorled Pogonia, Prickly Pear Cactus, and Cucumber Tree are species listed as Endangered. Wild Raspberry, Black-eyed Susans, Clover, Goldenrod, and Trilliums are widespread in forest ecosystems. Thickets and abandoned fields are h...
...e, and a quaint town only five minutes from the national park, there is always something to keep you entertained. As one of the last, nearly intact, temperate ecosystems on Earth it is home to a very unstable, diverse ecosystem. Come to this magnificently beautiful mountain range, and witness all its beauty and serenity first hand.
MacDougall, Brenda. One of the Family: Metis Culture in Nineteenth-Century Northwestern Saskatchewan. Vancouver: University of British Columbia Press, 2010.
The Athabasca oil sands are the second largest producer of crude oil in the world, with a surface area of approximately 100 000 square kilometres (Anderson, Giesy & Wiseman, 2010). The Alberta Energy and Utilities Board estimates that the oil sands contains approximately 1.7 trillion barrels of crude bitumen, however only 19% can be ultimately recovered (Raynolds, Severson-Baker & Woynillowicz, 2005; Humphries, 2008). The availability of recoverable bitumen makes Canada’s oil sands deposit larger even than that of Saudi Arabia (Czarnecki, Hamza, Masliyah, Xu & Zhou, 2004).The process of surface and in situ mining of the Athabasca oil sands is causing rapid and significant degradation of the regional environment surrounding Fort McMurray and the Athabasca River. Production is expected to increase to three million barrels per day by 2015 from approximately 2 million currently (Humphries, 2008). This increase will further exacerbate the existing environmental impacts of crude oil production. The Canadian oil and natural gas industry is extremely lucrative, but despite the short-term economic benefits of the mining of the Athabasca oil sands, the remediation of the negative environmental impacts of the extraction of oil on terrestrial and aquatic environments, biodiversity, and greenhouse gas emissions are a priority.
Canada is known for its natural resources and scenic wonders, such as the beautiful Niagara Falls, the great mountains and different climates. Canada is one of the best countries. to live, because of many factors: life expectancy, healthcare and GDP. leading in comparison to many other countries. Life expectancy is the most important reason that makes Canada a good place.