Silt.
loess: fertile, yellow-gray soil deposited by wind and water
Fine grained particles tightly packed by wind due to erosion are called loess. Loess deposits can be found in areas where wind has transported and deposited silt-sized particles, creating a distinctive and fertile soil.
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.
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 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.
loess: fertile, yellow-gray soil deposited by wind and water
Fine grained particles tightly packed by wind due to erosion are called loess. Loess deposits can be found in areas where wind has transported and deposited silt-sized particles, creating a distinctive and fertile soil.
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.
Fine particles of fertile land that is deposited on the banks of a river after a flood
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 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.
shale is fine grained
fine grained
Fine grained has larger crystals and coarse grained has smaller crystals
Fine grained has larger crystals and coarse grained has smaller crystals
The period of time involved in the rock cycle which would involve the transformation of a coarse grained rock into weathered, eroded, transported, deposited, and cemented fine-grained sedimentary particles would vary greatly. Suffice it to say the entire process would take many thousands-to-millions of years.
coarse grained