Geologists use both relative and absolute dating methods to determine the age of rocks and fossils. Relative dating involves determining if a rock is older or younger than another rock by examining their positions. Absolute dating determines the exact age by measuring the radioactive decay of isotopes using their half-life, or the time it takes for half of the radioactive atoms in a sample to decay. Common absolute dating techniques include radiocarbon dating and potassium-argon dating, which allow scientists to determine that the Earth is approximately 4.6 billion years old.