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Chapada Diamantina Canyon in Vale do Capão, Bahia Pictographs in Parque Nacional da Chapada Diamantina. Chapada Diamantina ([ʃaˈpadɐ dʒi.ɐmɐ̃ˈtʃĩnɐ]; Portuguese for the "Diamond Plateau") is a region of Bahia state, in the Northeast of Brazil. This mountain range is known as “Serra do Espinhaço,” in Minas Gerais state, south of ...
The Chapada Diamantina National Park (Portuguese pronunciation: [ʃaˈpadɐ dʒi.amɐ̃ˈtʃĩnɐ]; Portuguese: Parque Nacional da Chapada Diamantina) is a national park in the Chapada Diamantina [a] region of the State of Bahia, Brazil. The terrain is rugged, and mainly covered by flora of the Caatinga biome.
Palmeiras is a municipality in the state of Bahia in the North-East region of Brazil. [2]Palmeiras is an important tourist site in the Chapada Diamantina region. It is the site of the Vale do Capão (Capao Valley) or Caete-Açu, the Cachoeira da Fumaça (Smoke Falls) [3] and the Morro do Pai Inácio (Pai Inacio Hill), [4] among other landscape features.
View of the dissected plateau at Chapada Diamantina, Brazil. Shaded relief map of Cumberland Plateau and Ridge and Valley Appalachians on the Virginia/West Virginia border. A dissected plateau is a plateau area that has been severely eroded such that the relief is sharp.
Cachoeira da Fumaça is located in Palmeiras, Bahia, Chapada Diamantina, an attractive region for adventurers, named that way because the tiny water flow is sprayed by the wind before it touches the ground. However, depending on the season, it can be completely dry.
Chapada Diamantina National Park: The mount is 1,120 metres high and exists at the coordinates 12º27º'27"S 41º28'23"W History. A slave had a romance with a ...
The following other wikis use this file: Usage on ceb.wikipedia.org Vale do Capão; Usage on cs.wikipedia.org Global 200; Usage on de.wikipedia.org
A view of Chapada Diamantina National Park in Bahia, Brazil. A chapada (Portuguese pronunciation:) is a plateau found in the Brazilian Highlands.The chapadas, which are usually described as mountain ranges, are capped by horizontal strata of sandstone.