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The geological application of the carbon-14 method has made it possible to set a time scale for developments in the climate and vegetationof the Earth.
Even though it is very small, it is still possible to measure the carbon-14 atoms content in an organic material.
Because carbon-14 decays at this constant rate, an estimate of the date at which an organism died can be made by measuring the amount of its residual radiocarbon. The method is widely used by Pleistocene geologists, anthropologists, archaeologists, and investigators in related fields.
Geologists often need to know the age of material that they find.
In addition, the inventors of this method were honored with the Nobel Prize in Chemistry in 1960, as the method was revolutionary in today’s dating techniques.
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