Radiocarbon dating measures the decay of carbon-14 isotopes in organic materials to determine their age, typically within a range of 55,000-60,000 years. Developed in the 1940s by Willard Libby, this method revolutionized archaeology, environmental science, and climate research by providing accurate dates for wood, bone, pollen, and other organic remains. Today's Accelerated Mass Spectrometry (AMS)…
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