it is one of the alluvial plains
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An alluvial plain is a large flat landform that is created from the deposition of sediment or debris over a long period by rivers from the highlands. Sediments are brought about by weathering and erosion then water and wind transport the debris along. Once the deposited sediments increase, they form alluvial soil. The process of transporting the sediment by water is called fluvial process. Sediments are formed when there are floods which carry debris along the way. When the waters of the river subside, the sediments are deposited and with time an alluvial plain emerges.
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An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular period of time, whereas the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time.
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