A river always takes the easiest course through channels and soft
ground to the sea, flowing swiftly down mountain sides but much more slowly on
the level plains.
On the plain the river takes advantage of every difference in gradient.
This winding course is accentuated by the process of silting and erosion. As a
river flows round
a curve, the water on the outer bend moves more swiftly to cover the greater
distance in the same time as the water flowing
past the inner bend.
The more rapidly moving water will tend to wear away
the bank a of the channel, while the slow or movement of the water on the
inside wall will allow silting to take place. When the curve becomes more
pronounced it is known as a "meander". Notable examples of meanders
are to be found in the Wye in England, and the Meuse in France.
Sometimes the river erodes the bank so fiercely that a
new channel is formed, leaving an island of earth in the middle of the stream
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