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The Brazilian Highlands or Brazilian Plateau (Portuguese: Planalto Brasileiro) is an extensive geographical region covering most of the eastern, southern and central portions of Brazil, in all some 4,500,000 km 2 (1,930,511 sq mi) or approximately half of the country's land area.
Brazil map of Köppen climate classification zones Although 74% of the country is within the tropical zone , the climate of Brazil varies considerably from the mostly tropical North (the equator traverses the mouth of the Amazon) to temperate zones below the Tropic of Capricorn (23°27' S latitude), which crosses the country at the latitude of ...
The following outline is provided as an overview of and topical guide to Brazil: . Brazil – largest country in both South America and Latin America.With a geographical area of 8.5 million km 2, Brazil is also the largest country in the Southern Hemisphere and the world's fifth-largest country.
The results, published by the scientific American Journal of Human Biology by a team of the Catholic University of Brasília, show that, in Brazil, physical indicators such as colour of skin, eyes and hair have little to do with the genetic ancestry of each person, which has been shown in previous studies (regardless of census classification). [31]
Topographical map of Brazil. The Great Escarpment in Brazil is a major geological formation that runs along much of the eastern coast of Brazil south of the city of Salvador. The escarpment runs along the central and south Atlantic coasts of Brazil, rising sharply and separating the highland plateau from the coast. [1]
Highest in the states of Minas Gerais and Espírito Santo, Highest in the Brazilian Highlands: Pico do Cruzeiro: 2,861: 9,386 Unconfirmed elevation [1] Pico do Calçado: 2,849: 9,347 Pedra da Mina: 2,798: 9,180: Mantiqueira Mountains Highest in São Paulo state Pico das Agulhas Negras: 2,791: 9,157: Mantiqueira Mountains Highest in Rio de ...
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The basalt samples at Paraná and Etendeka have an age of about 132 Ma, during the Valanginian stage of the Early Cretaceous. [3] Indirectly, the rifting and extension are probably the origin of the Paraná and Etendeka traps and it could be the origin of the Gough and Tristan da Cunha Islands as well, as they are connected by the Walvis Ridge (Gough/Tristan hotspot).