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Meandering of a river refers to the winding, sinuous patterns that rivers create as they flow across landscapes, characterized by curves and bends. This phenomenon is primarily caused by erosion on the outer bank and deposition on the inner bank, where water flow velocity varies. While meandering increases the length of the river, nature counteracts this elongation through processes like sediment deposition and the eventual formation of oxbow lakes, which can redirect the river's flow and restore balance to the system.

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