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The process of radiocarbon dating starts with the analysis of the carbon 14 left in a sample.

The unstable and radioactive carbon 14, called radiocarbon, is a naturally occurring isotope of the element carbon.

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History, anthropology, and archaeology are three distinct but closely related bodies of knowledge that tell man of his present by virtue of his past.

When a living thing dies, it stops interacting with the biosphere, and the carbon 14 in it remains unaffected by the biosphere but will naturally undergo decay.

Decay of carbon 14 takes thousands of years, and it is this wonder of nature that forms the basis of radiocarbon dating and made this carbon 14 analysis a powerful tool in revealing the past.

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