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The four major divisions of time include Precambrian time, the Paleozoic Era, the Mesozoic Era, and the Cenozoic Era. The eras are further divided into periods.
Modern geologists believe that both the sudden events of catastrophism and the gradual changes of uniformitarianism play a role in geologic change.
Geologists use clues to determine what the Earth was like long ago. Scientists gather these clues from many different sources:
• fossils
• sedimentary rock
• tree rings
• ice cores
• seafloor sediment
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