The article explores the layers of rocks in the Konshisha area in southern Benue Trough. By studying the rocks, the researchers found three main types: sandy, limestone, and shale. The sandy rocks were likely formed in a shallow sea near a river, while the limestone rocks suggest a calm lagoon environment. The rocks show signs of being squished by tectonic forces, and the sandy rocks came from nearby. Overall, the findings suggest that the area went through a period of rising sea levels followed by a retreat, leading to the different types of rocks we see today.