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Chapada
A chapada () is a plateau found in the Brazilian Highlands. The chapadas, which are usually described as mountain ranges, are capped by horizontal strata of sandstone. They show the original surface, which has been worn away by the rivers, leaving here and there broad flat-topped ridges between river basins and narrower ranges of hills between river courses. From the valleys their rugged, deeply indented escarpments, stretching away to the horizon, they have the appearance of a continuous chain of mountains. See also * Chapada do Araripe * Chapada Diamantina * Chapada dos Guimarães * Chapada das Mangabeiras * Chapada dos Veadeiros Chapada dos Veadeiros National Park ( pt, Parque Nacional da Chapada dos Veadeiros) is a national park of Brazil located in the state of Goiás, on the top of an ancient plateau with an estimated age of 1.8 billion years. The park was created on ... References Escarpments Plateaus of Brazil Mountain ranges of Brazil {{topography-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapada Diamantina National Park
The Chapada Diamantina National Park (; pt, Parque Nacional da Chapada Diamantina) is a national park in the Chapada Diamantina region of the State of Bahia, Brazil. The terrain is rugged, and mainly covered by flora of the Caatinga biome. Location The park is in the Caatinga biome, and covers . It was created by decree 91.655 of 17 September 1985, and is administered by the Chico Mendes Institute for Biodiversity Conservation. The park covers parts of the municipalities of Palmeiras, Mucugê, Lençóis, Ibicoara and Andaraí in the state of Bahia. Terrain The park is in the Chapada Diamantina, a plateau bounded by cliffs of in central Bahia. Altitudes in the plateau typically vary from . In the more mountainous parts there are several peaks of , and a few over . The plateau forms a watershed, draining on one side into the São Francisco River and on the other into the De Contas River and Paraguaçu River. The park lies in the rugged Sincorá Range in the east of the plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapada Do Araripe
The Chapada do Araripe, also known as the Serra do Araripe, is a ''chapada'' (plateau) in northeastern Brazil. The chapada forms the boundary of Ceará and Pernambuco states, and forms the watershed between the Jaguaribe River of Ceará, which flows northward into the Atlantic, and the much larger basin of the São Francisco River of Pernambuco and neighboring states, which drains eastward into the Atlantic. The Santana Formation, which is rich with fossils from the early Cretaceous, lies at the base of the chapada. The Araripe manakin (''Antilophia bokermanni''), a bird only described in 1998, is endemic Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found else ... to Chapada do Araripe. Etymology The word "Araripe" stems from the Tupi word ''ararype'', meaning " macaw at the river" (''a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapada Dos Veadeiros
Chapada dos Veadeiros National Park ( pt, Parque Nacional da Chapada dos Veadeiros) is a national park of Brazil located in the state of Goiás, on the top of an ancient plateau with an estimated age of 1.8 billion years. The park was created on January 11, 1961 by President Juscelino Kubitschek, and listed as a World Heritage Site by Unesco in 2001. It occupies an area of in the municipalities of Alto Paraíso de Goiás, Cavalcante and Colinas do Sul. The park is maintained by Chico Mendes Institute for Biodiversity Conservation. History The Chapada dos Veadeiros region was first developed around the golden mine rush in the 18th Century. Cavalcante was one of the first villages founded in the region, and at one point became one of Brazil's major gold extractors. Some reports say that Isabel, Princess Imperial of Brazil visited Cavalcante, making it capital of the Empire for a day. The necessity of slave labor to work the mines in the Chapada dos Veadeiros was so great that th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapada Dos Guimarães
Chapada dos Guimarães is a municipality located in central Brazil, 62 km from the city of Cuiabá, the capital of Mato Grosso State. It is home to the Chapada dos Guimarães National Park. Outside this town is the geographic center of South America. The municipality contains 77% of the Rio da Casca Ecological Station, a strictly protected conservation unit created in 1994. The municipal seat contains the Quineira State Park, created in 2006. References External links Chapada dos Guimarães website Municipalities in Mato Grosso {{matoGrosso-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brazilian Highlands
The Brazilian Highlands or Brazilian Plateau ( pt, Planalto Brasileiro) are an extensive geographical region, covering most of the eastern, southern and central portions of Brazil, in all approximately half of the country's land area, or some 4,500,000 km2 (1,930,511 sq mi). In addition, the vast majority of Brazil's population (190,755,799; ''2010 census'') lives in the highlands or on the narrow coastal region immediately adjacent to it. Ancient basaltic lava flows gave birth to much of the region. However, the time of dramatic geophysical activity is long past, as there is now no seismic or volcanic activity. Erosion has also played a large part in shaping the Highlands, forming extensive sedimentary deposits and wearing down the mountains. The Brazilian Highlands are recognized for the great diversity to be found there: within the region there are several different biomes, vastly different climatic conditions, many types of soil, and thousands of animal and plant specie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapada Das Mangabeiras
The Chapada das Mangabeiras is a mountain range in central Brazil. The range runs northwest–southeast, and separates the basin of the Tocantins River to the southwest from the upper basin of the Parnaiba River to the northeast. The range also forms the boundary between Tocantins state and the states of Maranhão and Piauí Piaui (, ) is one of the states of Brazil, located in the country's Northeast Region. The state has 1.6% of the Brazilian population and produces 0.7% of the Brazilian GDP. Piaui has the shortest coastline of any coastal Brazilian state at 66&n .... The highest points of both states are located there. The points are unnamed locations, one measuring 804 meters (Maranhão), and the other, 860 meters (Piauí). References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Escarpments
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of Brazil
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
