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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.What we have initiated through our investigations is that in the U. there are several instances where a middle man becomes the victim to the scammer.These scammers are intellectual and are very familiar with their game.With the older and more resistant rocks of the Precambrian peneplain, these form a low, picturesque coastline of sandy bays and rocky promontories. Most of the other rivers, such as the Pra, the Ankobra, the Tano, and a number of smaller ones, flow directly south into the ocean from the watershed formed by the Kwahu Plateau, which separates them from the Volta drainage system.South of Kumasi, in the south-central part of the country, is Ghana’s only true natural lake— Over much of the surface of Ghana, the rocks are weathered, and great spreads of laterite (red, leached, iron-bearing soil) and lesser spreads of bauxite and manganese are found on the flat tops of hills and mountains.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).

Ghana, country of western Africa, situated on the coast of the Gulf of Guinea.

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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.

Kwame Nkrumah, who viewed Ghana’s sovereignty as being important not only for the Ghanaian people but for all of Africa, saying “Our independence is meaningless unless it is linked up with the total liberation of the African continent.” Indeed, more than 30 other African countries, spurred by Ghana’s example, followed suit and declared their own independence within the next decade.

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