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The geological eras are divided into four main eras: Precambrian, Paleozoic, Mesozoic, and Cenozoic. Each era represents a significant period in Earth's history characterized by distinct geological and biological events. These eras help scientists understand the evolutionary history and changes that have occurred on our planet over millions of years.
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geologic time scale
Eras, epochs, and periods are used in geology and paleontology to divide and categorize Earth's history based on major events or changes in the environment, life forms, or geological processes. This helps scientists understand the sequence of events and evolution of life on Earth over millions of years. It also provides a framework for dating and correlating rocks and fossils across different regions.
The Earth's history is divided into geologic time periods, with the largest unit being eons, which are further divided into eras, periods, epochs, and ages. The current eon we are in is the Phanerozoic eon, divided into the Paleozoic, Mesozoic, and Cenozoic eras. Each division represents significant changes in Earth's geological and biological history.