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.
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
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.
The proposed territory of the South Okanagan- Similkameen National Park Reserve is located in the South Okanagan and Similkameen Valleys in southern British Columbia, currently comprised of five Provincial Protected Areas. These areas include the 4700 hectare Mt. Kobau Site situated on the height of land between the Okanagan and Similkameen valleys; the 1850 hectare Chopaka East Site situated on Black Mountain, between Richter Pass and the International Boundary; the 470 hectare Chopaka West Site situated between Richter Mountain and the International Boundary; the 2350 hectare Kilpoola Site situated north and south of Highway 3 including the southeast slopes of Mount Kobau, Blue Lake and Kruger Mountain to the International Boundary; and the 25889 hectare Snowy Protected Area situated between the Lower Similkameen Indian Reserve. These areas, with the exception of Snowy Protected Area, compose the South Okanagan Grasslands Protected Area. Potential future additions of Crown and private lands would possibly see large tracts of land north and south of Mt. Kobau along with tracts north and east of the existing boundaries of Snowy Protected Area.
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.
...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 comparison between Belgium and Canada’s physical geography displays similarities and differences. A difference is the area Canada possesses which makes Canada the 2nd largest country in area. This massive area spanning across 6 different time zones, also has 6
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.
Galois, Robert M. “Upper Canada: Agriculture and Rural Settlement.” Lecture, University of British Columbia, Vancouver, November 10, 2011.
National Parks have awed tourists and even locals for years. They provide an escape from the ordinary and relief from the everyday stress of society. National Parks provide insight into a simpler time where our ancestors were surrounded by the beauty of nature instead of the concrete jungles of modern day metropolitan areas. Few of these wonderful parks provide the same seclusion as Denali National Park in Alaska. It’s sights and sounds have fascinated many and will continue to provide a great escape from everyday life.
Saskatchewan, one of the ever-growing and stunning provinces of Canada is a home to 1.12 million people. This wonderful place attracts thousands of immigrants per year from almost every corner of the world. Due to a huge count of immigrant arrival yearly, Saskatchewan holds Canada’s most rapidly developing economy as well.
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.
...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.
North, South, East, West and Central- there are definite qualities that detach Prairie from Maritimes, Ontario from Quebec and the Territories from the British Columbia. Each of these regions are separated by how they live, and their different culture background. Which forms our own identites within the counrty. Canadian and American government also show difference in how they govern themselves. United States is a country of one basic language. It has one main language, for its federal government and for every state. Canada is a country of two basic languages, French and English. A second basic difference between our Constitution and the American is that we are a constitutional monarchy and they are republics. For we have a parliamentary-cabinet government, while the Americans have a presidential-congressional. This means that the president is the head of the state and head of the government. While in Canada the Governor General is head of the provinces and the Prime Minister is the head of the government. Parliamentary-cabinet government is based on a concentration of powers. The Prime Minister must by custom be a member of one House or the other, or get a seat in the House. In the United States, the President and every other member of both houses are e...