Geologists determine the age of events in the geological past by relative dating (establishing which event comes first, usually by superposition and crosscutting relationships) and by numerical dating (obtaining a numerical age estimate on an event, usually by radioisotopic dating of interbedded or crosscutting igneous rocks). From these dating methods, geologists have determined that the earth is 4.5 billion years old, and that most events in the geological past took place millions to hundreds of millions of years ago.
Keywords: stratigraphy; geochronology; geological timescale; biostratigraphy; radioactivity





