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Take a look at this:

"In 1896 Henri Becquerel and Marie Curie discovered that certain isotopes undergo spontaneous radioactive decay, transforming into new isotopes. Atoms of a parent radioactive isotope randomly decay into a daughter isotope. Over time the number of parent atoms decreases and the number of daughter atoms increases. Rutherford and Soddy (1902) discovered that the rate of decay of a radioactive isotope depends on the amount of the parent isotope remaining. Later it was found that half of the parent atoms occurring in a sample at any time will decay into daughter atoms in a characteristic time called the half-life."

from http://myweb.cwpost.liu.edu/vdivener/notes/radiometric_dating.htm

These discoveries lead to the practical application of radiometric dating so you could probably credit the discovery to these individuals.

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15y ago
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4mo ago

Radiometric dating was discovered by scientists Bertram Boltwood in the early 20th century. Boltwood used the radioactive decay of uranium and thorium minerals to determine the age of rocks and minerals.

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Related questions

Is a geological dating method based on the decay rates of radioactive elements?

Radio metric dating.


What is the best method of radiometric dating?

Radiometric dating is the principal source of information about the absolute age of rocks and other geological features, including the age of the Earth itself, and can be used to date a wide range of natural and man-made materials.


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Carbon 14 dating is the best known example of radiometric dating, but there are many others. Another example of radiometric dating is the dating of the age of geological formations on earth. The oldest known rocks on the earth that have been analyzed, have been dated back some 4.404 billion years.


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Radiometric dating is the term for a method to determine the age of an object based on the concentration of a particular radioactive isotope contained within it. Example sentence:One of the early tests of radiometric dating was to estimate the age of the wood from an ancient Egyptian artifact, for which the age was already known from historical documents.


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