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The Cordilleran mountains were formed by the collision of the Pacific and North American tectonic plates causing the crust to buckle, creating the mountain ranges that are known today. This is the youngest of the three primary geographic regions of Canada, the others being the Canadian Shield and Interior Plains.
The precise boundaries of this cordillera and its subregions, as well as the names of its various features, may differ depending on the definitions in each country or jurisdiction, and also depending on the scientific field; this cordillera is a particularly prominent subject in the scientific field of physical geography. [3] [4]
The Pacific Coast Ranges are part of the North American Cordillera (sometimes known as the Western Cordillera, or in Canada, as the Pacific Cordillera and/or the Canadian Cordillera), which includes the Rocky Mountains, the Columbia Mountains, the Interior Mountains, the Interior Plateau, the Sierra Nevada, the Great Basin mountain ranges, and ...
Canada stretches from the Atlantic Ocean in the east to the Pacific Ocean in the west; to the north lies the Arctic Ocean. [1] Greenland is to the northeast with a shared border on Hans Island. To the southeast Canada shares a maritime boundary with France's overseas collectivity of Saint Pierre and Miquelon, the last vestige of New France. [2]
Cordillera Central of Luzon and Southern Pacific Cordillera of Mindanao in the Philippines Cordilleras Béticas , Central and Cantábrica (including the Picos de Europa ) in Spain East Australian Cordillera, more commonly known as the Great Dividing Range , the most significant topographic feature of the east coast of Australia
The Cordillera, in turn, is the eastern part of the Pacific Ring of Fire that runs all the way around the Pacific Ocean. View of Lake Louise in Alberta The Canadian Rockies are bounded on the east by the Canadian Prairies, on the west by the Rocky Mountain Trench, and on the north by the Liard River.
The Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, Canada , they run northwest from the lower stretches of the Fraser River to Bella Coola and Burke Channel , [ 1 ] north of which are the Kitimat Ranges .
On the West coast of North America, the coast ranges and the coastal plain form the margin, which is partially bounded by the San Andreas Fault, a transform boundary of the Pacific Plate. Most of the land is made of terranes that have been accreted onto the margin. In the north, the insular belt is an accreted terrane, forming the margin.