Carbon-14 dating is a radiometric dating method used to determine the age of organic materials by measuring the concentration of carbon-14 isotopes present. This technique relies on the principle of radioactivity, where carbon-14, a radioactive isotope of carbon, decays over time at a known rate, allowing scientists to estimate when an organism died based on the remaining amount of carbon-14 in the sample. The method is crucial for fields like archaeology and geology, providing insights into historical timelines and environmental changes.
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