Generally flat or low-lying areas that are adjacent
and run parallel to river channels and are covered by
water during flood stages of the river. The floodplain of a
river is built by alluvium carried by the river and deposited in
overbank environments, forming layers of silt, clay, and sand.
Overbank deposits are typically cut by many narrow elongate
channels filled by sands and gravels, marking places where
the river formerly flowed and meandered away during the
course of river evolution. Active and buried channels are typically
separated from the floodplain deposits by a sandy or
gravelly levee deposit, formed during flood stages of the river.
These form because the velocity of floodwater decreases
rapidly as it moves out of the channel, causing the current to
drop heavy coarse-grained material near the river, forming a
levee. Floodplains are also found around some lake basins
that experience flood stages.
Floodplains are being increasingly built upon, creating
potential and real hazards during floods. Floodplains are
characterized by fertile soils and make excellent farmlands,
which are nourished by yearly, decadal, and centurial floods,
whereas buildings, towns, and cities have a much more difficult
time dealing with periodic flooding.
See also FLOOD; GEOMORPHOLOGY; RIVER SYSTEM.
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