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.
Meandering channel from aerial
picture of Niger Delta. Picture from Francis Anwana.
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