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Chapada da Diamantina National Park

Chapada Diamantina National Park
IUCN category II (national park)
Chapada diamantina.jpg
Escarpments in the park
Map showing the location of Chapada Diamantina National Park
Map showing the location of Chapada Diamantina National Park
Location Bahia, Brasil
Coordinates 12°52′49″S 41°22′20″W / 12.88028°S 41.37222°W / -12.88028; -41.37222Coordinates: 12°52′49″S 41°22′20″W / 12.88028°S 41.37222°W / -12.88028; -41.37222
Area 152,142 ha (587.42 sq mi)
Designation National park
Created 17 September 1985
Administrator ICMBio

The Chapada Diamantina National Park (Portuguese: 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.

The park is in the Caatinga biome, and covers 152,142 hectares (375,950 acres). 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.

The park is in the Chapada Diamantina, a plateau bounded by cliffs of 41,751 square kilometres (16,120 sq mi) in central Bahia. Altitudes in the plateau typically vary from 500 to 1,000 metres (1,600 to 3,300 ft). In the more mountainous parts there are several peaks of 1,600 to 1,800 metres (5,200 to 5,900 ft), and a few over 2,000 metres (6,600 ft). 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 plateau, an area of folded and heavily eroded structures. The range is elongated in a north-south direction, and has an average width of 25 kilometres (16 mi). The highest point of the state is in the park, the 2,036 metres (6,680 ft) Pico do Barbado. Both gold and diamonds have been found in the range. The range forces moist air moving west from sea upward which causes higher levels of rainfall, particularly in the east. There are many systems of caves formed by the rivers of the region.


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