Soil and Geology

District: Sekondi-Takoradi Metropolitan

Last updated: June 3, 2025

The Sekondi-Takoradi Metropolis is characterized by faulted shale and sandstone resting on a hard granite basement, gneiss, and schist. The faulting system has a marked influence on the land formed, especially along the coastline, which clearly follows the main fault direction of North East.  

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