Normally, the profile of the land will diminish unless some counter force such as land uplift is operating.
Normally, the profile of the land will diminish unless some counter force such as land uplift is operating.
River sediments are deposited where gravity and friction acting on the sediments overcomes the force of the moving water. Often, this is on the inner bend of a meandering river, where water speed is the slowest, or at the mouth of the river where it enters a larger body of water.
deposition
An alluvial fan is typically formed at the base of a mountain or hilly area where a river or stream exits a narrow canyon or valley, and the water carrying sediments spreads out onto a flatter, open area. The fan shape is created as the water slows down and deposits the sediment it was carrying.
Alluvial deposits are river/stream deposits, whether they are found at the mouth of the river or anywhere along its length. In some cases, the alluvial deposits at the mouth of a river can form a delta.If this is not what you wanted to know, please rephrase the question. As it stands, this is an incomplete sentence with a question mark at the end of it.
no
Floodplain
Sedimentary rock is formed from sediments deposited in bodies of water. Examples of sedimentary rocks that can form in this way include limestone, shale, and sandstone. These rocks are typically composed of particles that have been weathered, transported, and compacted over time.
A thick deposit of windblown fine-grained sediments is called loess. This sediment is typically uniform, composed of silt-sized particles, and can be found covering large areas of land.
Legacy sediments are the upland, usually agricultural sediments, that have made their way into our stream and river systems in the post-colonial period (generally after 1700 CE). As the land was massively deforested, these soils ran off the land and accumulated in these stream valleys, sometimes behind mill dams or other in stream blockages, and now are actively eroding as stormwater driven flows scour these artificially narrowed conveyances. The erosion of these legacy sediments carries silt and nutrients, particularly phosphorus downstream, and eventually to tidewater, impairing water quality.
It could become a waterfall. Or if it just flows over onto more land then it becomes a river, not a stream.
well first is weathering, then the sediments ,then erosion takes the sediments to a new place ,then they are deposited there for a new land form to come