Radiocarbon dating is a scientific method used to determine the age of an artifact or fossil by measuring the amount of carbon-14 it contains. This technique is vital for understanding the timeline of archaeological and geological events, allowing researchers to place materials in chronological order based on their carbon content. As living organisms take in carbon from their environment, the ratio of carbon-14 to carbon-12 changes after death, making this method effective for dating organic materials up to about 50,000 years old.