Any unconsolidated, non-stratified soil composed primarily of silt-sized particles.
Loess is mainly composed of fine-grained sediment, such as silt and clay, that has been transported by wind and deposited over time. Its mineral composition can vary depending on the source material and the processes involved in its formation.
that would be know as loess: soil believed to be mainly deposited by wind
Loess is a type of sediment made of silt-sized particles that is typically deposited by the wind. It is known for its ability to retain moisture and nutrients, making it ideal for agriculture in some regions.
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.
The most common wind deposits are sand dunes and loess. Sand dunes are typically found in deserts and coastal areas, while loess deposits are made up of fine-grained sediments that are often found in regions with strong winds, like the Great Plains of North America and parts of China.
D. FINE SILT PARTICLES
Loess is mainly composed of fine-grained sediment, such as silt and clay, that has been transported by wind and deposited over time. Its mineral composition can vary depending on the source material and the processes involved in its formation.
that would be know as loess: soil believed to be mainly deposited by wind
Loess is a type of sediment made of silt-sized particles that is typically deposited by the wind. It is known for its ability to retain moisture and nutrients, making it ideal for agriculture in some regions.
The English word for Loess is actually also loess, a word that doesn't come up often in everyday speech. Loess means "A buff to gray windblown deposit of fine-grained, calcareous silt or clay" --credit to dictionary.reference.com
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 is deposited by wind.
Loess is a wind-blown sedimentary deposit. Good examples are found in China and Siberia. Loess (pronounced LOH ihs or lehs) is a kind of silt that forms a fertile topsoil in some parts of the world. Loess consists of tiny mineral particles brought by wind to the places where they now lie. These mineral particles are finer than sand, but coarser than clay. Topsoils that are made up of loess are found in the central and northwestern parts of the United States, in central and eastern Europe, in central Asia and east-central China, and in Argentina.
Loess is predominantly composed of silt-sized particles, typically quartz, feldspar, and mica. It is a wind-blown sediment that accumulates in layers, forming a porous and friable sedimentary deposit.
Loess could be considered a windblown soil.
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