deflate
An annually deposited sedimentary layer is called a varve. Originally the word referred only to those annual layers of sediment deposited in a lake by glaciers, but now the more general use is accepted. Another term used in the literature is "annually laminated."
The fine sediment left behind when a flood recedes is called silt. Silt consists of particles smaller than sand and is often deposited on floodplains as the water recedes.
The answer to that question is loess
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.
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.
An annually deposited sedimentary layer is called a varve. Originally the word referred only to those annual layers of sediment deposited in a lake by glaciers, but now the more general use is accepted. Another term used in the literature is "annually laminated."
Gypsum is a mineral that was formed by layers of sediment , fine particles, that were deposited over a period of time, and then subjected to geologic forces.
yes
sediment
Thick layers of fine sediment collect on them
The fine sediment left behind when a flood recedes is called silt. Silt consists of particles smaller than sand and is often deposited on floodplains as the water recedes.
The answer to that question is loess
The water flows through a mixed media filter with layers of layers of gravel, sand, and charcoal or coal, which filter out fine sediment. The sediment is removed from the filter by backwashing, dewatered and disposed of in a landfill.
Thick layers of fine sediment collect on them
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.
Fine sediment, such as silt or clay, can be carried far from its source by wind or water due to its low settling velocity. These fine particles can be transported long distances before settling out of suspension, leading to their presence far from the original source area.
The fine soil that was deposited at the mouth of a river in Egypt was called silt.