A second is equal to 52,083.3 years in geologic time, a minute to 3,125,000 years, and an hour to 187.5 million years.
The Earth's rock record serves as the foundation for the geologic time scale, often known as the geological time scale (GTS). It is a method of chronological dating that applies both geochronology and chronostratigraphy, which is the act of linking strata to time (a scientific branch of geology that aims to determine the age of rocks).
It is mostly used by Earth scientists to explain the sequence and linkages of events in the history of the Earth, including geologists, paleontologists, geophysicists, and geochemists. The time scale was created by examining the relationships between rock layers and their distinguishing characteristics, including lithologies, paleomagnetic traits, and fossils.
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