Canada geography is vast and diverse. Occupying the most of the northern portion of the North America, the world's second largest country in the total area after the Russia.
An immense territory between the Pacific Ocean to the west and the Atlantic Ocean to the east and the Arctic Ocean to the north, with the United States to the south and the northwest and the Arctic Ocean to the north, Greenland is to the northeast. Southern coast of Newfoundland lies Saint Pierre and Miquelon, an overseas collectivity of France.
Since 1925, Canada has claimed the portion of the Arctic between 60 W and 141 W longitude to the North Pole however, that claim is contested.
Canada covers 9,984,670 km and a panoply of the various geoclimatic regions. Canada encompasses vast maritime terrain, with the world's longest coastline of 202,080 kilometres. Physical geography of the Canada is widely varied.
Physical geography explain the geographic patterns of climate, vegetation, soils, hydrology and landforms and the physical environments that result from their interactions. The physical geography merges with the human geography to provide a synthesis of the complex interactions between the nature and the society.
Boreal forests prevail throughout the country, ice is prominent in northerly Arctic regions and through the Rocky Mountains and
the relatively flat Canadian Prairies in the southwest facilitate productive agriculture.
Mountain system of the western North America extending more than 4,827 km from northwest Alaska to the Mexican border.
The system includes the numerous ranges and forms the Continental Divide. Its highest elevation is Mount Elbert 4,402.1 m
in the central Colorado.
Great Lakes feed the St. Lawrence river where lowlands host much of Canadas population. Appalachian mountains old and deteriorate range of mountains, approximately 380 million years in age. Notable mountains in the Appalachians include Mount Jacques Cartier and Mount Carleton. The Appalachians are home to a rich endemic flora and fauna and are considered to have been nunataks during the last glaciation era.
Western Canada has many volcanoes and it is the part of the system of volcanoes found around the margins of the Pacific Ocean, which is called the Pacific Ring of the Fire. There are 200 young volcanic centers that stretch northward from the Cascade Range to the Yukon Territory. Five volcanic belts with different volcano types and tectonic settings. The Northern Cordilleran Volcanic Province was formed by faulting, cracking, rifting and the interaction between the Pacific Plate and the North American plate. Garibaldi Volcanic Belt was formed by the subduction of the Juan de Fuca Plate beneath the North American Plate. Anahim Volcanic Belt was formed as a result of the North American Plate sliding westward over the Anahim hotspot.
Volcanism occurred in the Canadian Shield. It collect over 150 volcanic belts that range from 600 million to 2.800 billion years old. Many of Canada's major ore deposits are associated with the Precambrian volcanoes. There are pillow lavas in the Northwest Territories that are about 2.6 billion years old and are preserved in the Cameron River Volcanic Belt. Pillow lavas in rocks over 2 billion years old in the Canadian Shield signify that great oceanic volcanoes existed during the early stages of the formation of Earth's crust. The Ancient volcanoes play an main role in estimating Canada's mineral potential. Volcanic belts bear ore deposits that are related to the volcanism. Euro StarThe Eurostar or Euro Star is a high-speed train service between London, Paris and Brussels.
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Great Lakes feed the St. Lawrence river where lowlands host much of Canadas population. Appalachian mountains old and deteriorate range of mountains, approximately 380 million years in age. Notable mountains in the Appalachians include Mount Jacques Cartier and Mount Carleton. The Appalachians are home to a rich endemic flora and fauna and are considered to have been nunataks during the last glaciation era.
Western Canada has many volcanoes and it is the part of the system of volcanoes found around the margins of the Pacific Ocean, which is called the Pacific Ring of the Fire. There are 200 young volcanic centers that stretch northward from the Cascade Range to the Yukon Territory. Five volcanic belts with different volcano types and tectonic settings. The Northern Cordilleran Volcanic Province was formed by faulting, cracking, rifting and the interaction between the Pacific Plate and the North American plate. Garibaldi Volcanic Belt was formed by the subduction of the Juan de Fuca Plate beneath the North American Plate. Anahim Volcanic Belt was formed as a result of the North American Plate sliding westward over the Anahim hotspot.
Volcanism occurred in the Canadian Shield. It collect over 150 volcanic belts that range from 600 million to 2.800 billion years old. Many of Canada's major ore deposits are associated with the Precambrian volcanoes. There are pillow lavas in the Northwest Territories that are about 2.6 billion years old and are preserved in the Cameron River Volcanic Belt. Pillow lavas in rocks over 2 billion years old in the Canadian Shield signify that great oceanic volcanoes existed during the early stages of the formation of Earth's crust. The Ancient volcanoes play an main role in estimating Canada's mineral potential. Volcanic belts bear ore deposits that are related to the volcanism. Euro StarThe Eurostar or Euro Star is a high-speed train service between London, Paris and Brussels.
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