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Atmospheric 14C, New Zealand[http://cdiac.esd.ornl.gov/trends/co2/welling.htm] and Austria[http://cdiac.esd.ornl.gov/trends/co2/cent-verm.htm]. The New Zealand curve is representative for the Southern Hemisphere, the Austrian curve is represent
 
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There are 6 summaries on Radiocarbon dating.

Encyclopedia and Summary Information
summary from source:
Carbon Dating Summary
760 words, approx. 3 pages
Carbon dating is a technique used to determine the approximate age of once-living materials. It is based on the decay rate of the radioactive carbon isotope C-14, a form of carbon taken in by all living organisms while they are alive. Before the...
summary from source:
Carbon Dating Summary
707 words, approx. 2 pages
Carbon dating is a technique used to determine the approximate age of once-living materials. It is based on the decay rate of the radioactive carbon isotope 14C, a form of carbon taken in by all living organisms while they are alive. Before the...
summary from source:
Radiocarbon Dating Summary
516 words, approx. 2 pages
Radiocarbon dating is a technique for determining the age of very old objects consisting of organic (carbon-based) materials, such as wood, paper, cloth, and bone. The technique is based on the fact that both stable and radioactive isotopes of carbon...
summary from source:
Carbon-14 Dating Summary
228 words, approx. 1 pages
method of age determination that depends upon the decay to nitrogen of radiocarbon (carbon-14). Carbon-14 is continually formed in nature by the interaction of neutrons with nitrogen-14 in the Earth's atmosphere; the neutrons required for this reaction...
summary from source:
Carbon-14 Dating Summary
147 words, approx. 1 pages
Method of determining the age of once-living material, developed by U.S. physicist Willard Libby in 1947. It depends on the decay of the radioactive isotope carbon-14 (radiocarbon) to nitrogen. All living plants and animals continually take in carbon:...
summary from source:
Radiocarbon dating Summary
3,229 words, approx. 11 pages
Radiocarbon dating is a radiometric dating method that uses the naturally occurring isotope carbon-14 (14C) to determine the age of carbonaceous materials up to about 60,000 years.[1] Raw, i.e. uncalibrated, radiocarbon ages are usually reported in...


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