The geological time scale is a system of chronological dating that relates geological strata to time. It is used by geologists, paleontologists, and other Earth scientists to describe the timing and relationships between events that have occurred during Earth's history.
The four eras of the geological time scale are:
Periods are subdivisions of eras, representing smaller units of time, while epochs are subdivisions of periods, representing even shorter intervals of time.
Fossils provide evidence of past life forms and help scientists determine the relative ages of rocks and the organisms that lived during different time periods.
By organizing Earth's history into distinct time intervals, the geological time scale allows scientists to study the sequence of geological and biological events that have occurred over millions of years, providing insights into the evolution of life and the changing dynamics of Earth's geology.