Levee
Deposition occurs along the coast when waves lose energy and are no longer able to carry sediment. As a result, the sediment is deposited along the coastline. This process is influenced by factors such as wave energy, sediment size, and coastal topography.
It depends on where the sediment is deposited. Not all sediment is deposited in a body of water. If the transport mechanism is a stream then the sediment can be deposited on the flood plain of the river or in a lake. If the sediment is deposited on the flood plain it will do two things. 1) The sediment of the flood plain will eventually lithify and 2) The river will continue to down cut and after X number of years the flood plain will no longer be subject to the flood waters of the river. At this point it is classified as a terrace (a flood plain of the past that is no longer inundated by flood water). The cycle basically starts over at this point with weathering and erosion processes breaking down and transporting the terrace sediment back into the river. If the sediment is transported to a lake, a delta will form. As the sediment is deposited in the lake the main channel of the river will extend out into the lake, this lowers the gradient of the main channel which slows the flow of water through the channel and allows for the deposition of sediment in the channel. When the main channel fills with sediment and no longer has the ability to channel all of the water from the river, dis-tributary channels will form these dis- tributary channels migrate across the delta transporting sediment as they go. Lithification takes place in the lower layers of the delta but this lithified sediment is only subjected to erosion during very high flows that are capable of transporting the sediment that covers the lithified layers.Basically, no matter where the sediment is deposited, it is subject to the processes which weathered and transported it to its current location.Wow really? these guys are just looking for a basic answer not an essay
wrack is the debris along the shoreline
Alluvial sediment:is clay or silt or gravel carried by rushing streams and deposited where the stream slows down. Alluvial deposition refers to this process.by which alluvium is thus deposited.
I would consider tiny pieces of rock carried by water to be sediment. Sediment is generally clay or sand particles, but any type of rock ground into fine particles can be carried by water. This may include igneous-type rocks (those that come from around volcanoes and the bottom of the ocean).
The buildup of sediment deposited along the channel of a river that helps keep it within its banks is known as "levees." Levees can form naturally through sedimentation during flood events, where the river's overflow deposits sediment along its edges. They can also be artificially constructed to enhance flood protection. These raised banks help contain the river, preventing it from spilling over into surrounding areas.
Levee
till deposited from glacier
An alluvial channel is a watercourse that is formed by the flow of a stream or river and contains sediment (alluvium) that has been formed by erosion and deposited along its bed and banks. These channels are typically found in floodplains and are dynamic in nature, shifting their course over time in response to changes in water flow and sediment transport.
Deposition occurs along the coast when waves lose energy and are no longer able to carry sediment. As a result, the sediment is deposited along the coastline. This process is influenced by factors such as wave energy, sediment size, and coastal topography.
wrack is the debris along the shoreline
Sediment that is carried by a stream along the bottom of its channel.
It depends on where the sediment is deposited. Not all sediment is deposited in a body of water. If the transport mechanism is a stream then the sediment can be deposited on the flood plain of the river or in a lake. If the sediment is deposited on the flood plain it will do two things. 1) The sediment of the flood plain will eventually lithify and 2) The river will continue to down cut and after X number of years the flood plain will no longer be subject to the flood waters of the river. At this point it is classified as a terrace (a flood plain of the past that is no longer inundated by flood water). The cycle basically starts over at this point with weathering and erosion processes breaking down and transporting the terrace sediment back into the river. If the sediment is transported to a lake, a delta will form. As the sediment is deposited in the lake the main channel of the river will extend out into the lake, this lowers the gradient of the main channel which slows the flow of water through the channel and allows for the deposition of sediment in the channel. When the main channel fills with sediment and no longer has the ability to channel all of the water from the river, dis-tributary channels will form these dis- tributary channels migrate across the delta transporting sediment as they go. Lithification takes place in the lower layers of the delta but this lithified sediment is only subjected to erosion during very high flows that are capable of transporting the sediment that covers the lithified layers.Basically, no matter where the sediment is deposited, it is subject to the processes which weathered and transported it to its current location.Wow really? these guys are just looking for a basic answer not an essay
It might get more narrow, I mean since they are rocks it will close the path more
An example of a sediment found along a stream is sand. Sand particles are typically larger than silt or clay and are commonly found in streambeds or along the banks of rivers and streams. They are transported by the flowing water and deposited when the flow velocity decreases.
Recent deposits by a river are known as alluvium, which can include a mix of rocks, gravel, sand, silt, and clay. These materials are carried by the river's current and eventually deposited along its banks or floodplains.
A meandering stream creates a broad, flat floodplain through erosion. The erosion process widens the channel and can create river cliffs along the outer banks. Sediment is also deposited on the inner banks, forming point bars.