Depositional landforms


A floodplain is an area of land which is covered in water when the river bursts its banks.

A floodplain forms due to both erosion and deposition. Erosion by meanders removes any interlocking spurs, creating a wide, flat area on either side of the river. During a flood, material being carried by the river is deposited (as the river loses its speed and energy to transport it). Over time, the height of the floodplain increases as material is deposited on either side of the river.

Floodplains are often agricultural land as the area is very fertile because it's made up of alluvium (deposited silt from a river flood).

A floodplain has fertile soil, a wide valley and gentle valley sides. The river meanders through eroded interlocking spurs and can form oxbow lakes.


Levees are elevated banks of deposited material at the sides of the river that stand above the level of the floodplain.

  • Levees occur in the lower course of a river when there is an increase in the volume of water flowing downstream and flooding occurs.
  • Sediment that has been eroded further upstream is transported downstream.
  • When the river floods, the sediment spreads out across the floodplain.
  • When a flood occurs, the river loses energy. The largest material is deposited first on the sides of the river banks and smaller material further away.
  • After many floods, the sediment builds up to increase the height of the river banks, meaning that the channel can carry more water (a greater discharge) and flooding is less likely to occur in the future.
During a flood, water flows over the banks and deposits silt. In between floods, slow moving river deposits silt in riverbed and levees. With each flood the levees are built up.