The geologic time scale is divided into several hierarchical units: eons, eras, periods, and epochs. Here’s a brief description of each:
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Eon: This is the largest division of geologic time, covering billions of years. The Phanerozoic is one of the most well-known eons that includes the current geological time.
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Era: This is the next subdivision of time following an eon. Eras can last tens to hundreds of millions of years. The Phanerozoic Eon is divided into three eras: Paleozoic, Mesozoic, and Cenozoic.
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Period: A period is a division of an era, lasting tens of millions of years. Each era is made up of several periods, such as the Jurassic Period in the Mesozoic Era.
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Epoch: The epoch is a subdivision of a period, lasting millions of years. For example, the Holocene is an epoch within the Quaternary Period.
In summary, the geologic time scale is organized in this hierarchical order: Eon > Era > Period > Epoch. Each level represents a decreasing length of time.