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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.The most outstanding are the Kwahu (Mampong) Scarp ( Kwahu Plateau) in the south and the Gambaga Scarp in the north.
The intervening coastal zone between eastern and western extremes contains patches of Devonian sediments (about 360 to 415 million years old).
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.
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).
In addition to being known for its lush forests, diverse animal life, and miles of sandy beaches along a picturesque coast, Ghana is also celebrated for its rich history—its habitation possibly dating from 10,000 —and as a fascinating repository of cultural heritage.
The country takes it name from the great medieval trading empire that was located northwest of the modern-day state until its demise in the 13th century.