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Living things move sediments and soil from one place to another. Plants break down things with mechanical weathering.
The particles in the sediments are cemented as pressure squeezes out water. The dissolved minerals in the water, usually silica or calcite, then become solid (crystallize), tying the particles together.
First of all there is weathering (erosion) of rocks at some place, they are carried away by wind or water at some other place and deposited there.Layers on layers are deposited to form sediments.
When pressure is applied to pieces of sediment, compaction takes place. Compaction is the process in which pieces of sediment are under severe pressure and it becomes solid rock. Therefore, pressure turns pieces of sediment into sedimentary rock.
Erosion.
The process of settling out and grading of sediments is known out deposition. This will commonly happen after erosion takes place.
erosion
Transportation.
weathering can break down rocks into sediments then erosion carries the sediments from one place to another. Last but not least deposition lies all the sediments down
Living things move sediments and soil from one place to another. Plants break down things with mechanical weathering.
Sediments move place to place by Erosion.
Sediments move place to place by Erosion.
Contraction
The process is fermentation which takes place under anaerobic conditions.
By burring into the bottom sediments
deposition
Oxidative phosphorylation, or in other words the end phase of the electron transport in aerobic respiration. 0.5O2 + H2 ---> H20