Sediment is dirt, rocks, and sand carried by a river.
Sediments, such as sand, silt, and clay, are fine bits of rock and soil that are deposited on land by a river. These sediments are carried by the river's current and then settle on the river banks and floodplains when the water slows down. Over time, these sediments contribute to the formation of fertile soil and landforms in river valleys.
Deltas are landforms formed at the mouth of a river where the river meets a body of water, such as a sea or ocean. Silt is a type of sediment that is commonly found in river deltas, as it is carried by the river and deposited in the delta. The accumulation of silt over time contributes to the growth and formation of delta landforms.
The soil that is deposited by a river to form landforms such as river bars and river deltas is called silt. A river delta is the name of the landform that is created the mouth of a river.
Wind-blown sediment is called loess. It is comprised of fine particles such as silt and clay that have been carried and deposited by the wind. Loess deposits can be found in various regions around the world.
The answer to that question is loess
The soil that is deposited by a river to form landforms such as river bars and river deltas is called silt. A river delta is the name of the landform that is created the mouth of a river.
It is silt.
The fine soil that was deposited at the mouth of a river in Egypt was called silt.
Suspended load
load
Clay particles are very fine grained and light weight, so easily carried along by flowing water.
A Nile Flood.
Loess
Sediments, such as sand, silt, and clay, are fine bits of rock and soil that are deposited on land by a river. These sediments are carried by the river's current and then settle on the river banks and floodplains when the water slows down. Over time, these sediments contribute to the formation of fertile soil and landforms in river valleys.
Deltas are landforms formed at the mouth of a river where the river meets a body of water, such as a sea or ocean. Silt is a type of sediment that is commonly found in river deltas, as it is carried by the river and deposited in the delta. The accumulation of silt over time contributes to the growth and formation of delta landforms.
Fine silt and mud are carried further downstream than heavier rocks and gravel. Which often results in muddy banks at the river mouth.
The soil that is deposited by a river to form landforms such as river bars and river deltas is called silt. A river delta is the name of the landform that is created the mouth of a river.