Sediment of smaller mass is easier for the power of wind to overcome the power of gravity in moving it from one place to another. Most sediment moved by wind that is tiny as sand.
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A floodplain is a flat region of land formed of river sediment and it is flooded during the rainy season each year.
Human beings may cause erosion by activities such as farming or games. They may also cause erosion by cutting down trees and other vegetation that act as windbreakers.
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They both based on the amount of energy that is released during earthquake
Erosion
during wind erection, sand and sediment may form a shape, commenly known as a "boner".
During erosion, sediment particles are created as rocks are broken down into smaller pieces through processes like abrasion, weathering, and transportation. These sediment particles are then carried away by water, wind, or ice to be deposited elsewhere.
During a flood, the type of erosion most likely to occur is known as water erosion. This occurs as the force of the water flow can break down and transport soil and rocks, leading to the removal of sediment from the landscape. It can result in channel incision, formation of gullies, and deposition of sediment in other areas.
Floodplains are typically formed by the deposition of sediments carried and deposited by rivers during floods, rather than erosion. Erosion can shape the landscape, but floodplains are mostly a result of the sediment deposition process.
Floods play a role in weathering, erosion, and deposition by carrying and transporting large amounts of sediment and rocks. During a flood, erosion occurs as flowing water removes and transports material. Deposition happens when the water slows down, causing sediment to settle. Overall, floods can accelerate the processes of weathering, erosion, and deposition by moving and redistributing Earth's materials.
well, as it is being transported it can be sorted by its size and sediment is often well sorted when it is moved a lot by wind or waves. poorly sorted sediment often results from rapid transportation perhaps by a storm, flash flood, or a volcanic eruption. Sediment left at the edges of glaciers is also poorly sorted.
Rain can cause both erosion and deposition. Erosion may occur when rainfall washes away soil and sediments, leading to the cutting of channels and formation of gullies. On the other hand, deposition can happen when rainwater carries sediments and deposits them in a different location, such as when a floodplain receives sediment during a heavy rainfall event.
A river stage with high flow velocity and volume, such as during flood events, typically causes the greatest amount of erosion. The force of the water carrying sediment and debris can lead to significant erosion of riverbanks and the riverbed.
Dams can prevent erosion by reducing the flow of water downstream, which helps to stabilize the riverbed and banks. The reservoir created by the dam can also act as a sediment trap, capturing sediment that would otherwise erode the riverbanks and surrounding areas. Additionally, dams can regulate water flow, preventing sudden surges that can cause erosion during heavy rainfall or flooding events.
Streams erode sediment primarily during times of high flow or flood events when the velocity and volume of water are increased. The force of the water helps carry and transport sediment downstream, causing erosion along the streambed and banks. Wind and ice can also contribute to sediment erosion in streams.
Sediment is typically deposited in bodies of water and low-lying areas during flooding events, when the water flow slows down and sediments carried by the water settle out due to gravity. Sediment can also be deposited gradually over time through erosion and weathering processes.