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The area later became known for growing cacao, the source of cocoa beans.
Introduced there in the late 19th century, cacao continues to provide an important export for Ghana.
Most of the remainder of the country consists of Paleozoic deposits (about 250 to 540 million years old), which are thought to rest on older rocks.
The Paleozoic sediments are composed mostly of beds of shales (laminated sediments consisting mostly of particles of clay) and sandstones in which strata of limestone occur in places.
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They occupy a large area called the Lake Volta, an artificial lake that extends far into the central part of the country behind the Akosombo Dam and covers about 3,275 square miles (8,500 square km).
Along the north and south, and to some extent along the west, the uplifted edges of the basin give rise to narrow plateaus between 1,000 and 2,000 feet (300 and 600 metres) high, bordered by impressive scarps.
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Forts and castles, many of which still dot the Ghanaian coast today, were constructed by Europeans to protect their trade interests.