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Along the eastern edge of the Voltaian Basin, and extending from the Togo border to the sea immediately west of Accra, is a narrow zone of folded Precambrian rocks running northeast to southwest, forming the Akwapim-Togo Ranges, which vary in elevation from 1,000 to 3,000 feet (300 to 900 metres).The highest points in Ghana are found there, including Mount Afadjato (2,903 feet [885 metres]), Mount Djebobo (2,874 feet [876 metres]), and Mount Torogbani (2,861 feet [872 metres]), all situated east of the Volta River near the Togo border.

Leaching is more pronounced in the wet south, while the formation of laterite is more widespread in the drier north.

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

These ranges are part of the Accra Plains, which are underlain by some of the oldest Precambrian rocks known—mostly gneisses (coarse-grained rocks in which bands containing granular minerals alternate with bands containing micaceous minerals); in places they rise above the surface to form inselbergs (prominent steep-sided hills left after erosion).

The only extensive areas of young rocks less than about 136 million years old are in the wide, lagoon-fringed delta of the Volta, about 50 miles (80 km) east of Accra, and in the extreme southwest of the country, along the Axim coast.

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