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The water usually flows fastest on the outside of the bend (meander) and flows the slowest on th einside of the bend.
A meander is a bend in the coarse of the water flow in a river. There is not a river recorded with the most meanders, although rivers with the most meanders are located in Africa.
the flow of the river.
Usually it is the upper reaches (often termed as mountain streams) that flow the fastest. In the lower, flatter valleys, rivers tend to slow down (except in spate, when the river is in flood)).
Because it has further to travel
Because the inside of the meander has deposited rocks and rubble building it up and making the water shallower whereas the outside of ther meander is being eroded by fast moving water.
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.
The river flows the fastest in the middle of the river.
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.
Meanders are twists and turns in a river flow. The Mississippi River has meanders because of the way the water eroded the edge of the land.
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.
A meander is described to as a river or stream with eroded banks such that it no longer flows in a relatively straight path, but instead is a winding path.