Meander case study geography

A river can be divided into the upper, middle and lower course. The long profile of rivers can be used to portray the gradients in each of the river courses. Overall, the long profile of rivers tends to be concave, with a more gentle slope towards the lower course river mouth. Deposition occurs when the river does not have enough speed to carry the load eg.
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HSC Ancient History Part 1: Core Study - Cities of Vesuvius - Pompeii and Herculaneum - Dux College

You seem to have disabled JavaScript. You should really enable it for this site but most things should work without it. This can be a consequence of either a fall in the amount of sea water or the land rising. Both are the result of the comings and goings of ice ages.
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You seem to have disabled JavaScript. You should really enable it for this site but most things should work without it. In the upper course of a river, its load is large and mainly transported by traction along the river bed. When flowing water encounters bedload, it is forced over it and downcuts behind the bedload in swirling eddie currents.
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Secondly, the river flows over shallow riffles — rocky shores, where velocity is slow — and deep pools — where velocity is fast. Thirdly, as the river flows faster in pools, it has more erosive power, and begins to wear away the river channel at the outside of the pool, creating a bend. Hydraulic action is when the force of the water dislodges and carries away the river bed and sides.
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