Long ridges of sediments alongside the channel of a river are called levees. They are created by the deposits which are made when a river overflows its banks.
The part of a river that is underwater when the river overflows its banks is called the flood plain.
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It is called flooding der what is the real term
Flood Plains
After a stream's discharge increases, it overflows its banks and a flood occurs.
Natural levees are formed when floodwaters deposit sediments along the banks of a river during periods of flooding. As the water slows and spreads, it drops its heaviest sediment load first, building up a mound of material that acts as a barrier against future flooding. Over time, these deposits create elevated ridges along the riverbanks that help to contain and control the flow of water.
silt and sediment onto the surrounding floodplain.
Natural levees form along the banks of rivers during times of flooding, when sediment-rich water overflows onto the floodplain. As the water slows down and spreads out, it deposits sediment along the river banks, building up natural levees over time. This process typically occurs during repeated flooding events over many years.
The area normally covered by water when a river overflows its banks is called the floodplain. This is the flat, low-lying area surrounding the river that is susceptible to flooding during periods of high water flow. Floodplains serve as a natural buffer to absorb excess water and reduce the risk of damage to nearby communities.
Floodplain