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According to the Köppen system, [1] Chile within its borders hosts at least seven major climatic subtypes, ranging from low desert in the north, to alpine tundra and glaciers in the east and southeast, tropical rainforest in Easter Island, Oceanic in the south and Mediterranean climate in central Chile. There are four seasons in most of the ...
The geography of Chile is extremely diverse, as the country extends from a latitude of 17° South to Cape Horn at 56° and from the Pacific Ocean in the west to the Andes in the east. Chile is situated in southern South America, bordering the South Pacific Ocean and a small part of the South Atlantic Ocean. Chile's territorial shape is ...
The Grey Glacier of Chile's Torres del Paine National Park is located in the Zona Austral natural region.. Because Chile extends from a point about 625 kilometers north of the Tropic of Capricorn to a point hardly more than 1,400 kilometers north of the Antarctic Circle, within its territory can be found a broad selection of the Earth's climates.
Prior to the arrival of the Spanish in the 16th century, northern and central Chile was under Inca rule while independent Mapuche inhabited south-central Chile. Chile declared its independence from Spain on 12 February 1818. Today Chile is one of South America's most stable and prosperous nations, a recognized middle power, and an emerging economy.
The matorral ecoregion contains the majority of Chile's population and its largest cities. The Central valley is Chile's main agricultural region, and the region is also subject to extensive grazing, logging, and urbanization. Grasses and other herbaceous plants introduced from the Mediterranean Basin have covered extensive areas of the ...
Chileans are bundling up with more clothes and clutching cups of hot coffee as the country faces the most intense cold snap in nearly 70 years, bringing winter weather in the middle of autumn.
In the Late Cenozoic, Chile definitely separated from Antarctica, and the Andes experienced a significant rise accompanied by a cooling climate and the onset of glaciations. The subduction interactions shaped four main morphostructures of Chile: the Andes , the Intermediate Depression , the Coast Range , and the Peru–Chile Trench off the coast.
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