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Fluvial Landforms - Caused by Deposition Simplified Revision Notes

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3.3.3 Fluvial Landforms - Caused by Deposition

Floodplains

infoNote

Floodplain: The area of land next to a river, which can flood.

  • During a flood:
  • Material carried by the river is deposited as the river loses speed and energy.
  • Height of the floodplain increases over time as material is deposited on either side of the river.
  • Agricultural Land:
  • Floodplains are often used for agriculture as the area is very fertile.
  • Fertility comes from alluvium (deposited silt from a river flood).
image image

Estuary

  • Where the river meets the sea.
  • The river here is tidal; when the sea retreats, the volume of water in the estuary is reduced.
  • When there is less water, the river deposits silt to form mudflats, which are important habitats for wildlife.
  • The land of an estuary is not very fertile, making it unsuitable for agriculture.
  • Estuaries create good habitats for wildlife.
Estuary

Estuary

Delta

  • Found at the mouth of large rivers (e.g., the Mississippi).
  • Formed when the river deposits material faster than the sea can remove it.
  • As the river approaches the sea, it loses energy and deposits material.
  • Sediment may be sorted, with the heaviest material deposited first.
  • Over time, more sediment is added, building up a land mass (delta) at the mouth of the river.
  • Strong tides can wash away sediment; if not, it will accumulate to form a delta.

Levees

  • Natural embankments along the edges of a river.

  • During a flood, eroded material is deposited over the whole floodplain.

    image
  • Heaviest material is deposited closest to the river channel as the river slows down.

  • Over time, deposited material builds up, creating levees along the edges of the channel.

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