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As animals and plants die over the years they get covered up and buried into soil. The soft parts of their bodies rot away leaving behind only the hard parts like bones and teeth. These hard parts lose their original mineral composition or structure. Their remaining parts either get recrystallized or replaced by other minerals such as silica and iron pyrites. This is called a fossil. Recrystallization means exchange of one chemical by another within the skeleton which results in a coarser, perhaps heavier structure. Many fossils consist of original hard parts of the animal as well as minerals taken from the surrounding rocks...
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