deposition
The carrying away of naturally broken down materials is called erosion. Erosion is the process by which soil, rock, or sediment is transported and deposited in another location by wind, water, or ice.
Erosion wears away sediments deposition, typically through the action of water, wind, or ice. These erosional forces transport sediments from one place to another, carrying them downstream or depositing them in new locations.
Sand is deposited on beaches by a variety of natural processes, including erosion of rocks and cliffs, wave action breaking down rocks into smaller particles, and rivers and streams carrying sediments to the coastline. These sediments are then moved along the coast by longshore drift and deposited on beaches when the energy of the waves decreases.
Floods cause weathering by carrying sediments and debris that can physically break down rocks and soil. They also cause erosion by transporting these sediments downstream, wearing away the land and changing the landscape over time. Floodwaters can both pick up and deposit sediments, which can lead to both weathering and erosion processes occurring along the flood's path.
In a muddy stream, sediment transport processes such as erosion, sedimentation, and deposition would likely dominate. The turbulent flow in the stream can cause erosion of sediment from the streambed, leading to the suspension and transport of the sediments downstream. Sediments can also settle out and deposit in areas of slow-moving water or when the flow velocity decreases.
The dropping of sediments by any agent of erosion is called deposition. This process occurs when the transporting capacity of the agent (such as water, wind, or ice) decreases, causing the sediments it was carrying to settle on the Earth's surface.
Streams and rivers cause erosion by carrying sediment and rocks downstream, gradually wearing down the land over time. When the velocity of the water decreases, sediments are deposited along the riverbanks and the riverbed, leading to the formation of riverbanks and floodplains.
Higher velocity of the stream increases erosion by carrying and transporting more sediments, which can wear away the streambed and banks more quickly. It also increases the force of the water, allowing it to break down and transport larger rocks and debris. Conversely, lower velocity streams erode more slowly.
Waves affect a shoreline by carrying and depositing sediments, which can contribute to erosion or accretion depending on the wave energy and direction. Strong waves can erode the shoreline by carrying away sediments, while gentler waves may deposit sediments, leading to beach formation.
Sediments move downstream through processes like erosion, transportation, and deposition by the force of water, wind, or ice. As water flows, it picks up and carries sediments, gradually depositing them as the energy of the water decreases. This continuous cycle of erosion, transportation, and deposition allows sediments to be transported downstream over time.
The carrying away of naturally broken down materials is called erosion. Erosion is the process by which soil, rock, or sediment is transported and deposited in another location by wind, water, or ice.
Erosion wears away sediments deposition, typically through the action of water, wind, or ice. These erosional forces transport sediments from one place to another, carrying them downstream or depositing them in new locations.
in erosion sediments are are deposited, in weathering sediments are taken away
Erosion
Waves cause erosion through impact by carrying sediments and smashing them against the coast. They also erode through abrasion, where sediments carried by waves grind against the coast, wearing it down over time.
Erosion is the transfer of material from one place to another place. Deposition is the settling of sediments to a resting place.
The mud deposits of deltas come from the erosion and transport of sediments from upstream sources by rivers. These sediments are carried by the river and eventually deposited at the river mouth where the flow velocity decreases, forming the characteristic delta landforms.