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 the Earth's history.
The geological time scale is divided into several eras, each of which is further divided into periods and epochs. The major divisions of the geological time scale are:
There are several key concepts to understand when studying the geological time scale:
When studying the geological time scale, consider the following tips:
With a solid understanding of the geological time scale, you will be better equipped to interpret the Earth's history and the changes that have occurred over millions of years.