transported soil
that would be know as loess: soil believed to be mainly deposited by wind
The term for wind-blown soil is "loess." Loess is a fine-grained, silty sediment that is transported and deposited by the wind. It is commonly found in regions with strong winds and arid conditions.
The term for soil that settles in water is sediment. Sediment is the material that is carried and deposited by water, wind, or glaciers.
Dust. "Aeolian" is the term that means carried by the wind. Where the soil settles out, that would be an aeolian deposition. Loess is a type of aeolian deposition where silt is transported by the wind and deposited. The soil in Iowa is formed, in part, from loess that came from the rock flour that blew off the glaciers during the last ice age.
Wind causes soil erosion by picking up and carrying loose soil particles away from the ground surface. As the wind moves across the land, these particles can be deposited in new locations, leaving the original area with less soil cover. This process can lead to the degradation of fertile soil, making it more susceptible to erosion.
Alluvial soil is the name of rich fertile soil deposited on the riverbank.
Soil deposited by water could be silt or mud.
Large boulders are not typically deposited by wind because they are too heavy to be carried long distances by wind erosion.
Loess soil is a fine-grained sediment that is predominantly composed of silt-sized particles deposited by the wind. It is known for its fertility and ability to retain water, making it valuable for agriculture. Loess soil is typically found in regions where glaciers have deposited fine-grained material during the last Ice Age.
The soil that is deposited is called silt. The landform that is often created by deposited silt at the mouth of a river is called a river delta.
Silt is a fine-grained fertile soil deposited by water.
The process you are referring to is called sedimentation. It occurs when soil and rock particles are deposited by wind, water, or ice, leaving them behind in a different location from where they originated. Over time, these deposited materials can accumulate and form sedimentary layers.