Nearly 2,000 kilometres of levees built along the Mississippi River over the past century helped protect cities and farmland from major floods.
About Levees:
A levee is a structure, either natural or artificial, built along the edges of a stream or river channel to prevent flooding of the adjacent land.
It can also be used to divert the river to increase land for construction.
In some countries, levees are used to prevent water from flowing inland from the sea or diverting the river's course, revealing fertile soil.
They can also be used to prevent rivers from overflowing into cities during storms.
They are very important features, but if they break, the consequences are disastrous.
How Do Levees Occur?
A majority of levees form from earth material.
The flow of a water body pushes river sediments to the sides, thus creating a levee.
The riverbank forms a levee made of silk, sediment, and other material such as dead plants to the side as the water flows.
They stretch parallel to the river and control the flow.
Natural levees can be reinforced using artificial material.
In cases where levees do not exist, then artificial ones are constructed. They are made by piling rocks, sand, and soil along the riverbank.
When the river flow is too strong, they can be made of metal, wood, or plastic material. In some places, they are made of concrete.
Levees are constructed to a variety of heights and widths and with a variety of materials. The height or width of a levee often depends upon possible rain and storm events.
One of the largest modern systems of levees is that built along the Mississippi River In the central United States.
Sea Levees:
A majority of the leaves are used to control the flow of the river, but others are built along the coast.
The Netherlands is a prime example of how dams, levees, and dikes can be used to control tides.
The reclaimed land is then used for agricultural or residential use.
A levee was also constructed along the coast of the Bay of Fundy in Nova Scotia and New Brunswick in Canada to prevent high tides from flowing inland.
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