Wind transported sediment is known as "aeolian sediment."
The total sediment load transported by a stream is the sum of the bed load, suspended load, and dissolved load. Bed load consists of larger particles that roll, slide, and bounce along the streambed. Suspended load is finer particles carried in the water column, while dissolved load is material that is dissolved in the water itself.
A fan-shaped pattern of sediment deposit is typically caused by sediment being transported by a river or stream and then spreading out as the flow slows down at the point where the river meets a larger body of water, such as a lake or ocean. The slowing of the flow causes the sediment to settle and form the fan-shaped deposit.
igneous rock
Ferrigenous sediment originates from the erosion of iron-rich minerals, such as hematite and magnetite, in rocks on land. This sediment is then transported by rivers and streams to the ocean, where it can accumulate on the seafloor.
Deposition, whereby the sediment load being transported is dropped.
matter
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matter
Sediment that is carried by a stream along the bottom of its channel.
The greater the time that stream sediment is transported, the greater the probability that the sediment will become more rounded and well-rounded due to abrasion and attrition processes.
Matter
sand
Sediment transported in a stream can cause abrasion by acting as a kind of sandpaper, physically rubbing against and wearing away the surface of rocks and other materials in the stream's bed and banks. The force of the moving water and sediment can increase the rate of abrasion, particularly in areas with high sediment loads or fast-flowing currents. Over time, this abrasion can result in the erosion and shaping of the stream's channel.
The sediment that moves along the bed of a stream is called bedload. Bedload consists of larger particles such as sand, gravel, and boulders that are transported by rolling, sliding, or bouncing along the streambed.
Wind transported sediment is known as "aeolian sediment."
Stream load refers to the amount of sediment and materials that are being transported by a stream. It can consist of sand, silt, gravel, and organic matter, and is influenced by factors such as stream velocity, discharge, and erosion within the watershed. Monitoring stream load is important for understanding sediment transport and its impact on water quality and ecosystems.