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Slough (hydrology) : ウィキペディア英語版 | Slough (hydrology) A slough is a wetland, usually a swamp or shallow lake, often a backwater to a larger body of water. Water tends to be stagnant or may flow slowly on a seasonal basis. In North America, a slough can be a side-channel from or feeding a river, or an inlet or natural channel only sporadically filled with water.〔(Oxford Dicionaries Online )〕 An example of this is Finn Slough on the Fraser River, whose lower reaches have dozens of notable sloughs. ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Slough (hydrology)」の詳細全文を読む
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