Identification of the sensitive regions to soil erosion can be the foremost step in controlling
the vigorous pace of soil degradation in agricultural lands. This study employs individual …

The response of landforms to tectonic deformative processes can be effectively understood
by using geomorphic indices. The objective of this study is to evaluate the extent of …

Morphometric studies coupled with geophysical investigations from petroliferous basins
provide valuable information about tectonics of the regions. We deduce six morphologic …

Abstract The Garoua-Gaschiga Region (GGR) is a portion of the Cameroon passive margin
located North of Cameroon (Central Africa), inside the Cretaceous Benue Triple Junction …

The establishment, development and abandonment and/or destruction of ancient
civilizations were catalytically controlled by geomorphic features such as lakes and rivers …

Abstract The Edea-Eseka region (EER), a portion of West African Margin located in SW
Cameroon between 3° 30′—4° 00′ N and 10° 00′—10° 55′ E and submitted to …

The age of discovery and exploration (fifteenth-sixteenth century CE) in Europe and later
colonisation of newly explored territories by Portuguese, Spanish, Danish, French, Dutch …

The impact of climate change on rainfall patterns and intensity necessitates an accurate
estimation of runoff from rainfall to effectively manage water resources. This study utilized …

The present study has attempted to evaluate the morphometric characteristics of the fifth-
order sub-basins in the Kallar watershed of the Bhavani Basin. Morphometry is the science …

Abstract The Douala-Buea Region (DBR; 4°–5° N, 9°–10° 30′ E), a portion of the southern
Cameroon passive margin, developed on the Proterozoic granito-gneissic basement and …