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The relative dating techniques are very effective when it comes to radioactive isotope or radiocarbon dating.
Chronometric or calendar dating is a better choice.
Using these methods, the scientist determines a date range for when an event took place rather than where it fits in the overall record. The techniques scientist need for absolute dating did not become available until the later half of the 20th century.
Thus, the date of an artifact is relative to its location in the levels.
Our planet inherits a large number of artifacts and monuments bestowed upon us by older historic civilizations.
Chronometric techniques include radiometric dating and radio-carbon dating, which both determine the age of materials through the decay of their radioactive elements; dendrochronology, which dates events and environmental conditions by studying tree growth rings; fluorine testing, which dates bones by calculating their fluorine content; pollen analysis, which identifies the number and type of pollen in a sample to place it in the correct historical period; and thermoluminescence, which dates ceramic materials by measuring their stored energy.