A stream's sediment load is typically deposited, eroded, and redeposited many times in a stream channel, especially during climatic variations such as flooding. Sediments are deposited throughout the length of the stream as bars or floodplain deposits. At the mouth of the stream, the sediments are usually deposited in alluvial fans or deltas, which represent a lower-energy, more "permanent" depositional environment that is less susceptible to changes in the stream flow.
i got this from clift notes
I don't know I never tasted and I will never .
the poet campares
No.
Edward Pyddoke has written: 'Stratification for the archaeologist' -- subject(s): Archaeology, Methodology, Sedimentation and deposition
no, it is not real, only in one piece
Stream deposition occurs when a flowing stream loses energy, causing it to slow down and deposit sediment that it was previously carrying. This commonly occurs when the stream enters a flatter area, like a floodplain or a lake. As the stream's velocity decreases, it can no longer transport sediment, leading to deposition.
stream turns into green water
Deposition of stream load occurs when the velocity of the stream decreases, causing the stream to lose the energy needed to carry sediment. As a result, sediment particles are deposited on the streambed or banks. This typically happens in areas where the stream's slope decreases or the stream widens.
rate of stream discharge is directly proportional to the erosion i.e the higher the velocity of the stream then it will erode the rock rapidly while the deposition process will be slow when the velocity will be high.
stream turns into green water
Deposition is dominant in areas of a stream where the flow rate decreases, such as at the inner bends of a meander or near the mouth of the stream where it enters a larger body of water. In these locations, the stream has less energy to transport sediment, leading to deposition of the sediment it is carrying.
deposition
A stream deposition occurs when, in the lower reaches, the flow of water (speed of flow) is reduced. Which is when the heavier sediment falls out and settles on the river bed.
Thats what i wanted to know
i think you mean stream meander. the process is deposition
Deposition creates landforms such as alluvial fans and deltas.It can also add soil to a river.Hope this helps.
Decrease in stream velocity