A stream, which flows in a channel, is formed as a result of erosion as the channel itself must be formed from erosion. Deposition is not common here, but there is a lot of loose material in the stream which is eroded over time, which has been put there through erosion. The material is first eroded further, then transported, and will ultimately be deposited at the mouth.
kettle is a result of erosion though the material is an ancient deposition
A characteristic that exists at an erosion-deposition interface in a stream where equilibrium occurs is a balanced sediment load. This means that the stream has enough energy to transport sediment in erosion zones, but also deposits sediment in deposition zones due to reduced energy. This equilibrium results in a stable channel shape and flow pattern.
A crevasse forms as a result of erosion. It is a deep crack or fissure in a glacier caused by movement and stress, rather than a location of deposition of sediment.
Loess is a result of deposition. It is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust.
A steeper slope in a stream increases the velocity of the water, leading to increased erosion of sediment and rocks. This results in greater transportation of material downstream. Conversely, a gentler slope decreases the velocity of the water, causing less erosion and more deposition of sediment.
kettle is a result of erosion though the material is an ancient deposition
deposition
deposition
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 horn is erosion
erosion
Thats what i wanted to know
Yes. Since dunes are the result of erosion, they are categorized as deposition.
it will turn to snow
kettle is a result of erosion though the material is an ancient deposition
A characteristic that exists at an erosion-deposition interface in a stream where equilibrium occurs is a balanced sediment load. This means that the stream has enough energy to transport sediment in erosion zones, but also deposits sediment in deposition zones due to reduced energy. This equilibrium results in a stable channel shape and flow pattern.