Geologists have at their disposal an accurate method of dating rocks that can even cope with ages as far back as the origin of the Earth some 4.7 billion years ago.
The method is based on the fact that radioactive isotopes of chemical elements decay at a constant rate which is entirely independent of any environmental influences such as temperature or pressure.
A fundamental concept in this work is that of the half-life which refers to the length of time that elapses before half of a quantity of isotope has decayed to its end-product.
The most commonly used radioactive isotopes are shown in the table below, with their decay products and half-lives.
The ratio of decayed to undecayed isotope in a rock gives a measure of its age. It is evident from the huge figures for the half-lives of the isotopes that this technique is well able to produce a time-scale to include even the Earth’s oldest rocks.
|Radioactive isotope||Isotope name||Decay product||Decay product name||Half-life (billion years)
One billion is
one thousand million: