Calibrating the radiocarbon clock
Carbon-14 decays at a steady, predictable rate, which makes it look like a simple stopwatch for dating ancient wood, bone, or charcoal. However, the amount of radiocarbon in Earth's atmosphere has varied over the millennia, so an accurate date relies on calibrating the measurement against tree rings and other materials whose calendar age is already known.
Questions you could explore
- How do known-age samples help calibrate a measurement?
- Why can the result remain a range of possible dates?
Start reading
- Oxford Radiocarbon Accelerator Unit, University of OxfordRadiocarbon dating
Oxford’s radiocarbon unit explains dating, calibration, and uncertainty.
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