A hydrologist analyzing satellite imagery of Nigeria observes a drainage network where short tributary streams flow down parallel ridges and join the main stream almost at right angles, controlled by alternating bands of hard and soft folded sedimentary rocks. In which of the following physical regions of Nigeria is this trellis drainage pattern most prominently developed?
- The folded sedimentary belt of the Benue TroughCevap
- BThe upper crystalline basement complex of the Jos Plateau
- CThe low-lying coastal floodplains of the Niger Delta
- DThe flat alluvial plains of the Sokoto-Rima basin
Cevap
The folded sedimentary belt of the Benue Trough
The correct option is the folded sedimentary belt of the Benue Trough. Trellis drainage patterns form in regions with folded sedimentary topography where softer strata weather into parallel valleys while resistant strata form ridges. Tributaries cut through weak rock belts and join the master stream at right angles along fault lines and fold axes, which is characteristic of the Benue valley sedimentary structure.
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Anahtar Kavram
Structural control of drainage patterns in Nigerian physical regions