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Geological Formation

Chapada Diamantina

Sedimentary and Stratigraphic Formations

Chapada Diamantina is a mountainous highland region within the Espinhaco Range in the central Brazilian state of Bahia, built from ancient sedimentary quartzite and sandstone laid down over a billion years ago and later uplifted into a rugged plateau of table mountains, deep canyons, caves and waterfalls. The area takes its name from the diamonds mined there through the nineteenth and early twentieth centuries. A large part of the region is protected as Chapada Diamantina National Park, established in 1985.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Chapada Diamantina

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Chapada Diamantina
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Chapada Diamantina
Sources
1. Chapada Diamantina (Wikipedia)
Lead
Quote, Lead
In 1985, the Chapada Diamantina National Park was created with its headquarters in Palmeiras.
View the Source
Wikidata: Chapada Diamantina
Wikidata Q1062622, class allow-list match (w-wdresolver-0926)View the Source
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