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Carbon dating
method used to determine the age of an object containing organic material by measuring the amount of carbon-14 is left after decay
when the organism is alive, the ratio of carbon-14 to carbon-12 is equal but after it dies, the carbon-14 decays
Parent isotope
original radioactive material
Daughter isotope
stable, end-product of the radioactive decay
Decay curves
graphical representations of the decay of radioactive isotopes over time, illustrating the relationship between parent and daughter isotopes
Half life
the time required for half of a radioactive substance to decay into its daughter isotopes