They gradually get smaller
Water, wind, gravity, and ice can all move sediments from one place to another.
erosion
sediments, rocks, till, debris, and soil
Sediments have been transported over time through various natural processes such as erosion, weathering, and transportation by wind, water, glaciers, or gravity. These processes can move sediments from one location to another, shaping landscapes and depositing sediments in different environments. Eventually, these sediments can be compacted and cemented together to form sedimentary rocks.
Glacial deposits may form when glaciers move along mountains and break off sediments. These deposits can include a variety of sediment types such as till, moraines, and erratic boulders. As the glacier moves, it erodes and transports these sediments, eventually depositing them once the glacier melts.
The rocks will gradually get smaller
How do sediment move
Sediments are deposited mainly due to the action of gravity, erosion, and transportation mechanisms such as water, wind, and glaciers. As these agents move sediment particles, they eventually settle in locations where the energy of the transporting agent decreases, like riverbeds, lake bottoms, or the ocean floor. Once the energy decreases sufficiently, the sediment particles are no longer kept in suspension and are deposited.
Water, wind, gravity, and ice can all move sediments from one place to another.
Sediments move around due to the combination of the force of gravity acting on the sediment and or the movement of the fluid in which the sediment is entrained. Movement may either be made by air, water or ice. Sediment movement in fluids occurs in water bodies as a result of water currents and tides. (I have edited this article completely as the las idiot who type is they turn in to poo)
The force that is responsible for moving sediments in a river is the current.
It's where the plates of the lithosphere move around on, the plastic like layer of the asthenosphere. the plates move around on these
they get excited and move around faster
The process in which sediments move slowly downhill, is called creep. It is common where freezing and thawing occur. As ice expands in soil, it pushed sediments up. Then as soil thaws, the sediments move farther downslope. Over time, creep can move large amounts of sediment, possibly causing damage to some structures
erosion
The second image shows sediments in motion. The movement is likely caused by the flow of water or the force of gravity on the slope where the sediments are located.
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.