How is the geologic time scale divided into eons, eras, periods, epochs, and ages?

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The geologic time scale serves as a standardized calendar for Earth's history, subdividing time into hierarchical units based on stratigraphy—the classification and correlation of rock strata. In descending order of duration, these units are eons, eras, periods, epochs, and ages.1

The boundaries between these intervals are primarily delineated by the fossil record, specifically the emergence and disappearance of widespread species within rock layers. Because life has undergone continuous evolutionary changes, these biological markers allow scientists to correlate strata globally.12

While the relative order of these units is established through biostratigraphic boundaries, the scale is also numerically quantified using radiometric dating methods, such as the analysis of isotope pairs like potassium-argon or uranium-lead. This dual approach—combining relative chronostratigraphic sequences with absolute chronometric dates—provides the framework used by the International Commission on Stratigraphy to maintain the standard geologic time scale.123