THE GEOLOGY AND GEOMORPHOLOGY OF GULLY DEVELOPMENT IN AGULU-NANKA AND ITS ENVIRONS, SOUTHEASTERN NIGERIA.

Student: Faith Chinyere Obetta
Supervisor: Miss Onyekwelu I
HOD: Dr Okolo Chinenye Margaret
Department of Geological Sciences
Physical Sciences
Nnamdi Azikiwe University, Awka, Anambra State

Abstract

Gully erosion is recognized as one of the most destructive forms of land degradation in southeastern Nigeria, with Anambra State—particularly the Agulu–Nanka erosion complex—being severely affected. Unlike sheet or rill erosion, which remain relatively shallow, gully erosion develops deep and steep-sided channels that enlarge quickly, causing extensive damage to farmland, settlements, and infrastructure (Ofomata, 1985; Egboka, 1993). The Agulu–Nanka complex has been described as one of the most catastrophic erosion sites in West Africa, posing serious threats to thousands of residents

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