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Since the 1950s, geologists have used radioactive elements as natural "clocks" for determining numerical ages of certain types of rocks. "Forms" means the moment an igneous rock solidifies from magma, a sedimentary rock layer is deposited, or a rock heated by metamorphism cools off.

It's this resetting process that gives us the ability to date rocks that formed at different times in earth history.

The method compares the abundance of a naturally occurring radioactive isotope within the material to the abundance of its decay products, which form at a known constant rate of decay.

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Isochron plots for the rubidium-strontium system applied to old rocks from Greenland and for chrondritic meteorites.

In practice great care is necessary in applying isotopic methods to date rocks.

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A key assumption is that a sample has remain a closed system so that the number of parent and daughter atoms can be fully audited.

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