A radiometric dating technique uses the decay of dating the jjang

Radiometric dating, often called radioactive dating, is a technique used to determine the age of materials such as rocks.

It is based on a comparison between the observed abundance of a naturally occurring radioactive isotope and its decay products, using known decay rates.

So, we rely on radiometric dating to calculate their ages.This chain eventually ends with the formation of a stable, nonradioactive daughter nuclide.Each step in such a chain is characterized by a distinct half-life.In this case, U238 is the “parent” and Pb206 is the “daughter.” Scientists begin by measuring how long it takes for a parent isotope to decay into a daughter isotope.In this particular case, it takes 4,460,000,000 years for half of a sample of U238 to decay into Pb206.

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With that being said only organisms the are younger than 50,000-60,000 years old.

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