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The geography of South America contains many diverse regions and climates. Geographically, South America is generally considered a continent forming the southern portion of the landmass of the Americas , south and east of the Colombia–Panama border by most authorities, or south and east of the Panama Canal by some.
The culture of these regions were heavily influenced by the South American cowboy, known as the gaucho. Rioplatense region – Argentina, Uruguay, Brazil, and parts of Paraguay . This region, due to extensive immigration from Europe, mainly from Italy , Spain , and Portugal maintains a very European culture in terms of cuisine, art ...
The geography of western South America is dominated by the Andes mountains; in contrast, the eastern part contains both highland regions and vast lowlands where rivers such as the Amazon, Orinoco and Paraná flow. Most of the continent lies in the tropics, except for a large part of the Southern Cone located in the middle latitudes.
The following outline is provided as an overview of and topical guide to South America. South America is the southern continent of the two Americas, situated entirely in the Western Hemisphere and mostly (about 3/4) in the Southern Hemisphere. It lies between the Pacific and Atlantic oceans.
In parts of Europe and Latin America, America is considered to be a single continent, within which North and South America are regions. [ 2 ] Physical geography
Latin America is defined according to cultural identity, not geography, and as such it includes countries in both North and South America. Most countries south of the United States tend to be included: Mexico and the countries of Central America , South America and the Caribbean .
Map of Latin America and the Caribbean. The term Latin America and the Caribbean (LAC [1]) is an English-language acronym referring to the Latin American and the Caribbean region. The term LAC covers an extensive region, extending from The Bahamas and Mexico to Argentina and Chile.
The northern portion of the Arid Diagonal is a result of the blocking of the trade winds by the barrier formed by the Central Andes and the South Pacific High. [5] To the south in the westerlies, the rain shadow that the Southern Andes cast over eastern Patagonia similarly blocks moisture. [1]