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As the river winds from side to side, it tends to erode the outer bank and deposit sediment on the inner bank of the bend. Over time, the meander becomes more and more curved.

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Q: When does a river devlop meanders?
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Why do meandering rivers occur in humid areas?

Meandering characterized a river's course when its flow begins to slow. Meanders form when slight irregularities in the flow cause the moving water to be directed towards a bank. This bank then erodes and at this point the river gets wider and the flow slows causing sediment to be deposited against the opposite bank. Eventually the process causes a large bend in the river and the river develops meanders.


What are physical characteristics of a river?

The physical characteristics of a river vary according to age. In a young river, one would expect to find a steep gradient (slope), high discharge, rapids, steep sides, no floodplain, and a lot of downcutting. In a mature river, one would expect to find a medium gradient, meadows, some meanders (bends in the river path), a narrow floodplain, lateral erosion, and medium discharge. In an old river, one would expect to find large meanders, a wide floodplain, more lateral erosion, and low discharge.


What are the stages of a river?

the three stages of a river are- the upper course or the mountain stage- in this stage the river undergoes the mountains that are really very steep so the river has freat cutting power in this stage. the main work of the river in this stage is erosion and transportation. the middle course or the plain stage- the ground becomes less flat and the river slows down. the river becomes very smooth , but still it erodes some of the rocks. in the end of the middle stage , deposition takes place. the lower course or the delta stage- in this stage, the river slows down completely and forms a delta.


What would best describe a river with a meander?

meander in general is a bend in a sinuous watercourse. A meander is formed when the moving water in a river erodes the outer banks and widens its valley. A stream of any volume may assume a meandering course, alternatively eroding sediments from the outside of a bend and depositing them on the inside. The result is a snaking pattern as the stream meanders back and forth across its down-valley axis. When a meander gets cut off from the main stream, an oxbow lake is formed. Over time meanders migrate downstream, sometimes in such a short time as to create civil engineering problems for local municipalities attempting to maintain stable roads and bridges.There is not yet full consistency or standardization of scientific terminology used to describe watercourses. A variety of symbols and schemes exist. Parameters based on mathematical formulae or numerical data vary as well, depending on the database used by the theorist. Unless otherwise defined in a specific scheme "meandering" and "sinuosity" here are synonymous and mean any repetitious pattern of bends, or waveforms. In some schemes, "meandering" applies only to rivers with exaggerated circular loops or secondary meanders; that is, meanders on meanders.Sinuosity is one of the channel types that a stream may assume over all or part of its course. All streams are sinuous at some time in their geologic history over some part of their length


Where is the velocity greatest with a stream with meanders?

On the outside. This is because when the water is flowing around a meander, the water practically goes around, where erosion occurs. If you know science, wherever in a stream where erosion occurs, thats where the velocity is greatest.