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See also: embankment which keeps a See also: river in its channel
.
A river such as the See also: Mississippi (q.v.), draining a large See also: area, carries a See also: great amount of sediment from its swifter See also: head-streams to the See also: lower ground
.
As soon as a stream's velocity is checked, it drops a portion of its load of sediment and spreads an alluvial See also: fan in the lower See also: part of its course
.
This deposition of material takes place particularly at the sides of the stream where the velocity is least, and the See also: banks are in consequence raised above the See also: main channel, so that the river becomes lifted bodily upwards in its See also: bed, and flows above the level of the surrounding country
.
In See also: flood-See also: time the muddy See also: water flows over the river's banks, where its velocity is at once checked as it flows gently down the See also: outer See also: side, causing more material to be deposited there, and a long alluvial See also: ridge, called a natural See also: levee, to be built up on either side of the stream
.
These ridges may be wide or narrow, but they slope from the stream's outer banks to the plain below, and in consequence require careful watching, for if the levee is broken by a " See also: crevasse," the whole See also: body of the river may pour through and flood the country below
.
In 1890 the Mississippi near New See also: Orleans broke through the Nita crevasse and flowed eastward with a current of 15 M. an
See also: hour, spreading destruction in its path
.
The Hwang-ho river in See also: China is peculiarly liable to these inundations
.
The word levee is also sometimes used to denote a See also: riverside quay or landing-place
.
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