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 .
No.
the poet campares
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
stream turns into green water
stream turns into green water
deposition
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.
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
Deposition creates landforms such as alluvial fans and deltas.It can also add soil to a river.Hope this helps.
i think you mean stream meander. the process is deposition
Decrease in stream velocity
deposition
On the inner curve of a meander, where the velocity of the water is the slowest.