Scientists use two methods to determine the age of fossils - relative dating and absolute dating. Relative dating involves determining if one fossil is older or younger than another fossil without an exact age. Absolute dating determines a specific numerical age by measuring properties like the amount of carbon-14 or potassium-argon in igneous rocks and fossils. Scientists can use carbon-14 dating on fossils less than 60,000 years old and potassium-argon dating on fossils and rocks over 60,000 years old.