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"Let's not forget about the middle and the lower part of the stream. At the middle part of the stream, the meandering and the serpentine order of the stream is less frequent, because of the force of the stream. During this time, the river tries to flow in a straight-like manner, and in effect, causes ox-bow lakes. 'Se mo nyinaa kai owo no?' This time 'etese nea owo no eda ho na yede sekan atwitwa nemu.' Then it will be left with different pieces. At the lower part of the stream, the volume of the river becomes voluminous, carrying more debris, and these debris are deposited to form swampy areas called Aluvia Fan. "fan, fan, 'Enti papa nso monhu?" "

Mr. Festus Attakora-Mensah
former Geography teacher & later Butler Housemaster


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