Flat land near the edges of rivers formed by mud and silt deposited by floods is called a delta. There are several deltas around the world.
Alluvial soils are formed by the deposition of sediments carried by rivers and streams. Since these sediments are typically deposited by rivers, alluvial soils are also referred to as riverine soils. They are known for their fertility and are found in areas where rivers deposit sediments during floods or over time.
The soil or sediments itself is called silt, and the landform that is often created at the mouths of rivers is called a river delta. Sand bars are also created in rivers and other waterways by deposited silt.
Soil rich in minerals deposited by flooding rivers is called silt.
The fine yellow soil deposited after floods is likely to be silt. Silt is a sediment that is composed of smaller particles than sand, typically sourced from rivers and carried by water during flooding events. It is often deposited on floodplains and can contribute to the fertility of the soil.
Deltas are formed at the mouth of a river where it meets a body of water, typically the ocean, and consists of sediment deposited by the river. Floodplains are flat, low-lying areas adjacent to rivers that are prone to flooding and are formed by sediment deposited during floods. Deltas are specifically found at the river mouth, while floodplains extend along the sides of a river.
You could be thinking of a delta or abyssal plains.
Floodplains are typically formed by the deposition of sediments carried and deposited by rivers during floods, rather than erosion. Erosion can shape the landscape, but floodplains are mostly a result of the sediment deposition process.
Alluvial soil is carried and deposited from rivers, streams, and floodplains. It is formed by the erosion and weathering of rocks and minerals upstream, which are then transported and deposited by flowing water.
Land formed from sediment build-up is called a delta. Deltas usually form at the mouth of rivers where sediment, such as sand and silt, is deposited as the water slows down and spreads out.
Alluvial soil is formed where transported sediment is deposited. This type of soil is created by rivers and streams carrying particles and depositing them over time, resulting in a fertile soil that is good for agriculture.
The sediment itself is called silt, and it often is deposited at the mouth of rivers and forms a landform called a river delta.
The Advantages of Flooding are: -Formation of natural banks. -Formation of flood plains. -Rise in underground water table.