Dating methods are ways to determine the age of archaeological artifacts, fossils, or geological formations. There are many different dating methods, each with its strengths and limitations. Some of the most common dating methods include radiocarbon dating, dendrochronology (tree-ring dating), and thermoluminescence dating. These methods rely on different principles, such as the decay of radioactive isotopes, the growth patterns of tree rings, or the accumulation of radiation-induced electrons in minerals. By combining multiple dating methods, researchers can establish more precise and accurate chronological frameworks for understanding the history of human populations, environmental changes, and geological events.