As the rate of flow decreases, the rate of deposition increases
A delta is formed by deposition. Deltas are landforms that are created where a river meets a body of water, like an ocean or a lake. As the river flows into the larger body of water, it slows down, causing sediment it was carrying to settle and build up over time, forming the delta.
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.
No. A lava flow is considered an extrusive feature.
Deposition is dominant in areas of a stream where the flow rate decreases, such as at the inner bends of a meander or near the mouth of the stream where it enters a larger body of water. In these locations, the stream has less energy to transport sediment, leading to deposition of the sediment it is carrying.
The slope of land can affect the rate of deposition in a delta by influencing the speed of the river flow. A steeper slope can lead to faster river flow, carrying more sediment downstream, which can result in increased deposition. Conversely, a gentle slope may slow down river flow, allowing sediment to settle out more easily and potentially decrease deposition rates.
You could increase the amount of water flow, or increase the angle of water flow to increase the amount of erosion. Both will increase the amount of the resultant deposition.
A slope and the force of gravity.
Erosion carries sediments downstream, depositing them when the flow slows near a river mouth. Deposition builds up sediment, creating a triangular-shaped landform called a delta where the river meets a body of water like an ocean or lake.
Erosion carries sediment downstream, and when the water flow slows as it reaches a body of water like a river or ocean, deposition occurs. The sediment settles and accumulates, building up landforms like deltas. The continual cycle of erosion and deposition helps form the intricate network of channels and sediment buildup that characterize a delta.
The waters from Tennessee ultimately flow into the Gulf of Mexico. This occurs via several rivers, such as the Tennessee River, which joins the Ohio River, and ultimately the Mississippi River that empties into the Gulf of Mexico.
Aquifers are not a source of erosion or deposition. They are underground layers of rock or sediment that hold water, which can flow through them. Aquifers can be eroded by the slow movement of water through them over time, but they do not cause erosion or deposition themselves.
A split can be formed by both erosion and deposition. Erosion processes like weathering and water flow can create splits in rocks or landforms, while deposition of sediments can also fill in gaps and create splits in formations.