Geologist use radiodating to help determine ages of rocks and subsequently an estimate for the age of the Earth. It has been practiced and tried since when Clair Patterson first estimated the age of the Earth. Although radiodating can be a complicated topic, this essay looks to break down the basics of radiodating and examples of how radiodating is used in geology. The basis of understanding geological radiodating breaks down into Physics and Chemistry. First, isotopes of elements are atoms that have a different number of neutrons than other atoms of the same element.
half-life | Definition & Facts | Britannica
Comparisons between the observed abundance of certain naturally occurring radioactive isotopes and their decay products, using known decay rates, can be used to measure timescales ranging from before the birth of the Earth to the present. For example measuring the ratio of stable and radioactive isotopes in meteorites can give us information on their history and provenance. Radiometric dating techiques were pioneered by Bertram Boltwood in , when he was the first to establish the age of rocks by measuring the decay products of the uranium to lead. Carbon is the basic building block of organic compounds and is therefore an essential part of life on earth. Natural carbon contains two stable isotopes 12 C Radiocarbon dating was developed in the s, with Willard Libby receiving the Nobel Prize in chemistry for the use of 14 C to determine age in archaeology, geology, geophysics and many other branches of science. For many years it was assumed that the content of 14 C in the atmosphere was constant.
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If you want to know how old someone or something is, you can generally rely on some combination of simply asking questions or Googling to arrive at an accurate answer. This applies to everything from the age of a classmate to the number of years the United States has existed as a sovereign nation and counting as of But what about the ages of objects of antiquity, from a newly discovered fossil to the very age of the Earth itself? Sure, you can scour the Internet and learn rather quickly that the scientific consensus pins the age of of the planet at about 4. But Google didn't invent this number; instead, human ingenuity and applied physics have provided it.
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