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| | Dating Exhibit |
 | | Radiocarbon determinations can be obtained on wood; charcoal; marine and fresh-water shell; bone and antler; peat and organic-bearing sediments, carbonate deposits such as tufa, caliche, and marl; and dissolved carbon dioxide and carbonates in ocean, lake and ground-water sources. |
 | | In addition, the half-life of radiocarbon must be known with sufficient accuracy, and it must be possible to measure natural levels of radiocarbon to appropriate levels of accuracy and precision. |
 | | To measure the age (that is, the abundance of radiocarbon), the sample can be placed into a mass spectrometer and that atom counted, or the sample can be placed into a Geiger counter and counted, requiring a wait on the average of 8000 years (the mean life of radiocarbon) for the decay. |
| www.mnsu.edu /emuseum/archaeology/dating/radio_carbon.html (700 words) |
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