loess.
The resulting deposit is called loess.
A thick deposit of windblown fine-grained sediments is called loess. This sediment is typically uniform, composed of silt-sized particles, and can be found covering large areas of land.
A thick deposit of windblown fine-grained sediments is called loess. Loess is typically composed of silt-sized particles that have been carried by the wind and deposited over time, creating distinct layers of sediment. Its properties make it a fertile soil that is often used for agriculture.
Loess
Water can deposit sediment such as sand, silt, and clay. Wind can deposit smaller particles like sand and dust. Melting glaciers can deposit a mixture of rocks, sediments, and debris known as moraines.
A windblown deposit of fine dust is known as loess. Loess is typically made up of silt-sized particles that have been carried by the wind and deposited in layers. It is common in arid or semi-arid regions and can play a significant role in soil formation and fertility.
loess it is pronounced as less
The sediments with a mixture of sizes are known as poorly sorted sediments. This means that the particles have not been sorted by size and can range from fine to coarse within the same sediment deposit.
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
A deposit of windblown sand is referred to as a sand dune. Dunes occur naturally along coastlines. A manmade barrier of sand with some kind of landfill under it is referred to as a berm.
abrasion. This occurs when windblown particles like sand and dust wear away rock surfaces through friction. Over time, this constant impact can lead to the sculpting of landforms such as sand dunes.
It's just known as an Eolian (wind-driven) deposit. It will result in the formation of a slope of varying degrees, depending on the friction of the material against itself. Greater friction will lead to a slope of greater angle.