The geologic time scale is a framework used by geologists to represent Earth's extensive history, divided into eons, eras, periods, and epochs based on significant changes in rocks and fossils. Earth’s history spans approximately 4.6 billion years, with major periods such as Precambrian, Paleozoic, Mesozoic, and Cenozoic highlighting the evolution of life forms from early single-celled organisms to the present day. The current geological epoch is the Holocene, part of the Cenozoic era, which continues to the present and is often referred to as the age of man.