The process of erosion (removal of material) is not the same as the process of deposition (the adding of material).
As they are two separate processes, deposition is not a part of the overall erosion process.
However, without eroded sediments, there would be nothing to deposit, the two processes are therefore sequential (and part of the overall encompassing rock cycle processes).
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.
A drought can lead to decreased vegetation, which can increase weathering and erosion due to less protection from roots and vegetation to stabilize the soil. Additionally, water flow is reduced during a drought, leading to less deposition of sediment in riverbeds and coastal areas. Overall, a drought can intensify weathering and erosion processes while decreasing deposition rates.
A flood plain is primarily created by deposition. When a river overflows its banks during periods of high flow, it drops sediment and debris on the surrounding flat area, building up layers over time. While erosion may shape the flood plain by cutting into it, the main process of flood plain formation is deposition.
Erosion, Transportation, Deposition
Deposition is the process where matter changes from a gas to a solid. This occurs during cooling. When referrring the deposition as a weather process, water vapor forms into ice.
During mass movement, the transport phase, the load can be deposited and indeed can cause scouring. However the transport phase itself is only minimally linked to the initial erosion of the load or its final deposition.
Erosion. Weathering is the physical and chemical breakdown of rock. Erosion is the removal of of weathered sediments. Transport is the movement of weathered sediments (say in suspension in river water) during the erosion process. Deposition is the laying down of the transported sediments in a new location.
A floodplain is primarily formed by deposition. When a river overflows its banks during periods of high flow, it deposits sediment on the surrounding flat land, creating a floodplain. Erosion can also play a role in shaping the floodplain by cutting into the surrounding landscape.
Erosion. Weathering is the physical and chemical breakdown of rock. Erosion is the removal of of weathered sediments. Transport is the movement of weathered sediments (say in suspension in river water) during the erosion process. Deposition is the laying down of the transported sediments in a new location.
Deposition, the depositing of fine silt and animal carcasses on the floor of lakes and seas, has nothing to do with the slow erosion by water (freezing and flowing) and wind of boulders into pebbles.
Energy is not released during the process of deposition. Deposition is the phase transition in which a gas transforms directly into a solid without passing through the liquid phase. Energy is actually absorbed during deposition, as heat is removed from the gas to convert it into a solid.