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This picture of the Nowitna River in Alaska shows two oxbow lakes – a short one at the bottom of the picture and a longer, more curved one at the middle-right. The picture also shows that a third oxbow lake is probably in the making: the isthmus or bank in the centre of the most prominent meander is very narrow – much narrower than the width of the river; eventually, the two sections of ...
Animation of the formation of an oxbow lake. A meander cutoff is a natural form of a cutting or cut in a river occurs when a pronounced meander (hook) in a river is breached by a flow that connects the two closest parts of the hook to form a new channel, a full loop.
The oxbow lake at Vynthala was identified in 1998 by a team of scientists led by Sunny George. Earlier the lake had a length of 2 kilometres, but now only about 200 meters remain as the rest of the area has been reclaimed. The total area of the lake is around 7 hectares.
Fallacy regarding formation of point bars [ edit ] An old fallacy exists regarding the formation of point bars and oxbow lakes which suggests they are formed by the deposition (dropping) of a watercourse's suspended load claiming the velocity and energy of the stream decreases toward the inside of a bend.
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Lake Kanyaboli is the largest oxbow lake in Kenya and the second largest in Africa, formed after River Yala disconnected from its course at the meander stage, leaving behind a U-shaped lake. The lake is found in Siaya County in western Kenya and is home to a variety of fish species that have almost disappeared from Lake Victoria , the country's ...