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Sedimentary rock is the dominant type of rock found in the interior plains. It is formed by the accumulation of sediments over time, such as sand, clay, and organic materials, which are then compacted and cemented together. Sedimentary rocks in the interior plains often include limestone, sandstone, and shale.
Canada's largest deposits of sedimentary rocks can be found in Alberta and Saskatchewan (the Great Plains area). Some of the minerals found inside of sedimentary rock include coal, oil, natural gas, and potash.
The bedrock of the interior plains is thick due to a continuous accumulation of sediments over millions of years. Factors such as erosion, deposition, and tectonic activity have contributed to the gradual buildup of sedimentary rock layers, resulting in the thick bedrock found in the region.
The Canadian Shield is a large geological region characterized by ancient rocks and extensive forests, covering a significant portion of Canada. In contrast, the Interior Plains are a vast region of flat or gently rolling terrain located to the west and south of the Canadian Shield. The Canadian Shield has more rugged topography and older rock formations compared to the relatively flat and younger sedimentary rocks found in the Interior Plains.
Oil and natural gas are found in the interior plains due to the region's geological history, which includes the accumulation of organic materials in sedimentary basins over millions of years. The compression and heating of these organic materials under layers of sediment transformed them into hydrocarbons. Additionally, the interior plains have favorable conditions for trapping these resources, such as porous rock formations and impermeable cap rocks that prevent the oil and gas from escaping. This combination of factors makes the interior plains a significant area for fossil fuel deposits.
Gold deposits are not typically found in the Interior Plains region of North America. The majority of gold deposits are found in mountainous regions where geological processes have concentrated the metal. The Interior Plains are known more for their agricultural and energy resources.
It's several thousand metres thick. It's thick because they contain much of the oil and gas found in Alberta and Saskatchewan.
The oldest fossils are typically found in the deepest sedimentary rock layers, which are located at the bottom of a rock formation. This principle is known as the law of superposition in geology, where older rock layers are found beneath younger ones.
1.Canadian Shield 2.Interior plains
The interior plains typically feature flat or gently rolling landscapes, with fertile soil and abundant rivers. These plains are typically found in the central part of continents and are ideal for agriculture and human settlement. The lack of significant elevation changes contributes to the plains' vast expanses.
A variety of wildlife can be found throughout the Interior Plains region. Some of the animals include mule deer, pronghorn antelopes, brown bears, wolves, and elks. These animals make this region their home because there is lots of space and food.
Protolith is a term used to describe the parent rock of a metamorphic rock. Conglomerate is a sedimentary rock that can be composed of clasts of sedimentary, igneous, or metamorphic rocks, or any number of combinations of all.