Abstract
Drainage basins play a major role in the understanding of process and form dynamics within a landscape and they are referred to as fundamental physical units recognized in hydro-geomorphological studies as having a network of inter-related attributes. Until recently, information about streams in humid tropics was limited to their description in relation to geological structure. There are gaps to fill as regards but not limited to the mechanics of how river channels and networks evolve, lithological units and channel network patterns. This study aims to provide an answer to the question ‘what role do lithology play in channel network orientation and pattern?’ Answers will be provided using slope–area curves, rose diagrams and background information on long profiles extracted from Digital Elevation Models, DEMs (30 m) within sub-basins in Upper Ogun River Basin. Six third-order basins were selected systematically and randomly for the study. Topographic properties were extracted using System for Automated Geoscientific Analysis (SAGA) version 4.0.0, a GIS software. RockWare software was used in creating rose diagrams for lineament patterns and channel networks. S–A plots show that within the bedrock channels, sediment is limited and processes operating within these channels are sometimes non-fluvial and are most often than not well defined. Therefore, transiting into bedrock channels could produce inflection points that are not quite distinct as slope–area solutions might not have enough to account for the inherent hydro-dynamic variations operating therein.
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Olusola, A.O., Onafeso, O.D., Fashae, O.A., Adelabu, S. (2022). Geomorphological Analyses of Third-Order Basins in Southwestern Nigeria. In: Shit, P.K., Bera, B., Islam, A., Ghosh, S., Bhunia, G.S. (eds) Drainage Basin Dynamics. Geography of the Physical Environment. Springer, Cham. https://doi.org/10.1007/978-3-030-79634-1_21
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