A river that flows in a distinct channel
which follows a winding, hence meandering path. Parts of a meandering channel
are the line following the deepest point, thalweg, the sandy deposits on the inside of the
bend, point bar, and the isolated oxbow lake, caused by the cut-off of a
meander loop. The meander loop migrates depositing the point bar, which make up
the reservoirs. This is culled from IPE HWU Petroleum Geoscience manual.
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Meandering channel from aerial
picture of Niger Delta. Picture from Francis Anwana.
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