A scientific dating method widely used in archaeology to estimate the age of any organic material, such as wood, seeds, or animal remains.
A scientific dating method widely used in archaeology to estimate the age of any organic material, such as wood, seeds, or animal remains. By measuring the proportion of the isotope carbon-14, which is radioactive and therefore decays over time, material can be dated to as far back as about 50,000 years.
By measuring the proportion of the isotope carbon-14, which is radioactive and therefore decays over time, material can be dated to as far back as about 50,000 years.