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Sediment

Horizontales
Stiff, sticky fine-grained earth, typically yellow, red, or bluish-gray in color and often forms an impermeable layer in the soil. It can be molded when wet, and is dried and baked to make bricks, pottery, and ceramics.
Eroded sediments that are carried as the stream flows.
The process that changes rocks to sediments and can also alter the chemical composition of a rock.
Caused by the impact of water striking the surface.
The process that occurs after erosion, and it is the laying down of sediments like soil and rocks that have been carried by wind, water, gravity, or ice.
Made up of rock and mineral particles that are smaller than sand but larger than clay. They feel smooth to your fingers but gritty in your mouth. Sheet erosion, Caused by the unconfined flow of water running across the surface.
Verticales
Air or water move sedimentary particles, and are able to keep them moving based on the velocity of the flow. The faster the medium flows, the greater ability it has to move larger particles.
A fragment of rock or mineral ranging in size from less than a micron (too small to see) to as big as an apartment block.
A loose substance, it's typically pale yellow- tan, it's the result of erosion of other rocks and it is present on beaches, riverbeds, deserts, sea beds etc.
Caused by water concentrating into innumerable, closely spaced small channels. Saltation, The process in which sand grains are picked up and transported by wind.
Large particles that have been eroded that can not be carried by the stream are pushed along the stream bed.
A flat level area surrounding the stream channel that is created by streams eroding the outer edges of the bank.