May not be stagnant, but could be called a Mortlake or an Oxbow lake
Sometimes a meandering river forms a feature called an oxbow lake. An oxbow lake is a meander that has been cut off from the river. An oxbow lake may form when a river floods. EW
Oxbow lake.
Oxbow lake
A river's flow tends to slow down on reaching a flat valley floor. It is here that the river may meander, creating bends and ox-bow lakes.
This is likely an oxbow lake, formed when a meander loop is cut off from the main river channel. The sand and gravel have been deposited in the oxbow lake due to reduced water velocity, creating a sediment buildup. Over time, vegetation may establish in the oxbow, further stabilizing the bank and bottom.
Naturally rivers erode & deposit silt & debris over time, millions of years, and this erosion will, by force of gravity, alter the course of the river. Where there is a large meander, a huge bend in the river course, erosion may be so dramatic that the meander will be cut & this will form a lake in the old river course. This type of semi cirular lake is called an Oxbow lake. It is a cut off meander.
An oxbow lake is a U-shaped body of water formed when a meander of a river is cut off from the main channel, typically during a flood. Over time, the oxbow lake may become isolated from the river and eventually fill in with sediment.
At times, particularly during floods, a river may form a meander cutoff, a new, shorter channel across the narrow neck od a meander. The old meander may be abandoned as sediment separates out from the new, shorter channel. The cutoff meander becomes a cresent-shaped ox-bow lake. With time, an ox-bow lake may be filled with sediment and vegitation.
No. Platypuses do not live in the water. They live in burrows they dig alongside freshwater sources. This may be a lake, a creek, a river or a billabong.
A river usually flows quickly in the upper course, as it is at a higher elevation - mountains streams, waterfalls, etc. In the lower course, it will slow down as the lower elevation means the slope is more horizontal. It is here that the river may start to meander across the valley floor, forming bends, oxbow lakes, and a flood plain.
An oxbow lake is formed when a meander erodes. The bend gets a sharper angle, forming a "neck" of land between the two bends of a meander. This will be eroded during flood, as the water is flowing faster over the top of it and into it. After a few floods, the neck will be broken through. The water will now flow through this path. The mouths of the old meander will get blocked up, as the flow at the edge is slower and deposition will occur. When these mouths are blocked up completely, an oxbow lake will have been formed.