may be transported, usually by water (or wind in the case of sand) anddeposited to form sediments. These become buried under later forming sediments and water or by major tectonic activity, and then become subjected to compression as enormous pressures are created deep in the crust from the weight of rocks or sediments above them.Over millions of years from the fragments of eroded pre-existing rocks, water is squeezed out and the particles cement together with the help of dissolved salts and silica…
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