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Therefore, the second timeline shows an expanded view of the most recent eon.

In a similar way, the most recent era is expanded in the third timeline, and the most recent period is expanded in the fourth timeline.

Corresponding to eons, eras, periods, epochs and ages, the terms "eonothem", "erathem", "system", "series", "stage" are used to refer to the layers of rock that belong to these stretches of geologic time in Earth's history.

Geologists qualify these units as "early", "mid", and "late" when referring to time, and "lower", "middle", and "upper" when referring to the corresponding rocks.

For example, the boundary between the Cretaceous period and the Paleogene period is defined by the Cretaceous–Paleogene extinction event, which marked the demise of the non-avian dinosaurs and many other groups of life.

Older time spans, which predate the reliable fossil record (before the Proterozoic eon), are defined by their absolute age.

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Eons are divided into eras, which are in turn divided into periods, epochs and ages.

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Geologic units from the same time but different parts of the world often look different and contain different fossils, so the same time-span was historically given different names in different locales.

For example, in North America, the Lower Cambrian is called the Waucoban series that is then subdivided into zones based on succession of trilobites.

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