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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.
Ghana’s administrative capital is the coastal city of Relief throughout Ghana is generally low, with elevations not exceeding 3,000 feet (900 metres).
The southwestern, northwestern, and extreme northern parts of the country consist of a dissected peneplain (a land surface worn down by erosion to a nearly flat plain, later uplifted and again cut by erosion into hills and valleys or into flat uplands separated by valleys); it is made of Precambrian rocks (about 540 million to 4 billion years old).
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Although relatively small in area and population, Ghana is one of the leading countries of Africa, partly because of its considerable natural wealth and partly because it was the first black African country south of the Sahara to achieve independence from colonial rule.