Erosion is the movement of sediments by wind, water, ice, and gravity. Transportation of sediments by rivers and streams is referred to as fluvial erosion.
sediment
The two primary sources of sediment for beaches are rivers and coastal erosion. Rivers transport sediments from the land and deposit them along the coast, while coastal erosion breaks down rocks and cliffs along the shoreline, contributing sediment to the beach.
Mature rivers carry large amounts of sediment along their lengths. This helps to shape the land and produce fertile farm lands.
River valleys have very fertile land, a result of rivers moving soil and sediment and depositing it in the valley. It also provides movement for people along the river.
Rivers carry sediment, which when deposited at the beach, increases the land. Similarly, rivers can carry sediment away from a beach, also changing its shape. These two forces can work together to effectively move sediment from one area of the beach to another. Similarly, storms also move sediment.
they go out to a ocean or lake depositing sediment along the way. (hope this is what you meant)
The dropping of soil and rocks by rivers is called sediment deposition. As rivers flow, they carry sediment downstream, which can accumulate and settle along the riverbed or on the floodplain. This process helps in shaping the landscape and forming features like river deltas.
it's called a slump.
Sediment can be moved by various agents such as wind, water, ice, and gravity. Wind can transport sediment particles in the air, water can carry sediment along in rivers and oceans, ice can transport sediment in glaciers, and gravity can cause sediment to move downslope in the form of landslides or rockfalls.
Fast moving water carries more sediment because it has more energy to erode and transport sediments from the surface of the earth. As water velocity increases, it can pick up and carry larger and heavier particles along with it.
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.
Deltas form along coastlines when rivers deposit sediment as they enter slower-moving bodies of water, such as oceans or lakes. The reduction in water velocity causes sediment to accumulate, creating landforms that can extend outward from the shoreline. Over time, these deposits can build up and create a diverse ecosystem, shaped by the interaction of freshwater and saltwater. The formation of deltas is influenced by factors such as the river's sediment load, tidal action, and coastal currents.