The geological time scale is a system used by geologists and paleontologists to organize Earth's history into chronological periods based on significant geological and biological events. It divides time into eons, eras, periods, epochs, and ages, allowing scientists to communicate about Earth's past in a standardized way. The scale reflects major changes, such as mass extinctions and the emergence of new life forms, providing context for understanding the evolution of the planet and its inhabitants over billions of years. Essentially, it serves as a framework for interpreting Earth's geological and biological history.
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