The mature stage of river development is characterized by flat flood plains where the river meanders and deposits sediment. In this stage, the river has a large volume of water and is more stable, leading to the creation of wide flood plains.
A plain is basically a large, flat area and flood plains are the large flat areas to either sides of rivers. These areas, when it rains so much that the river bursts its banks, are covered in water: flooded.
A plain is basically a large, flat area and flood plains are the large flat areas to either sides of rivers. These areas, when it rains so much that the river bursts its banks, are covered in water: flooded.
The flat, wide area along a river is called its flood plain. This is sometimes part of a larger area called the alluvial plain, which formed as the river shifted over time and deposited soil when it flooded.
It's called a 'flood plain'.
Meandering course: Old age rivers have a winding and meandering course with gentle gradients as they have eroded their valleys over time. Wide floodplains: Old age rivers typically have wide floodplains due to their ability to transport and deposit sediments over many years, resulting in a broad and flat area alongside the river.
Some low lying land types are:ValleyFarewellMarshLow pointHollowLow-lying areaSheltered spotCrooner JerryDellLow-lying wetland
Flood plains and plains are both flat expanses of land. Flood plains are low-lying areas near rivers that are prone to flooding, while plains are large, flat areas with minimal elevation changes. Both types of landforms are valuable for agriculture and settlement due to their fertile soil and access to water.
It is the flood plain.
A coastal plain is a streach of land along a seacoast which slopes down. In most cases it is an elevated part of the oceanfloor. A flood plain is the floor of river valley beyond the river bed. It is formed by mud, sand and silt
Flood plain
Flood plain