Presented is an overview of the traditionally used absolute dating techniques for Quaternary geomorphological complexes.
It is shown that they have a narrow range of coverage both as regards the time interval and with respect to the set of objects dated; therefore, they are unsuitable for age diagnostics of most geomorphological formations.
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The chronological utility of amino acid racemization has been studied in several genera of mollusks from more than 200 Quaternary marine localities along both the Atlantic and Pacific coasts of the United States.Particular isotopes are suitable for different applications due to the type of atoms present in the mineral or other material and its approximate age.For example, techniques based on isotopes with half lives in the thousands of years, such as Carbon-14, cannot be used to date materials that have ages on the order of billions of years, as the detectable amounts of the radioactive atoms and their decayed daughter isotopes will be too small to measure within the uncertainty of the instruments.Coins found in excavations may have their production date written on them, or there may be written records describing the coin and when it was used, allowing the site to be associated with a particular calendar year.In historical geology, the primary methods of absolute dating involve using the radioactive decay of elements trapped in rocks or minerals, including isotope systems from very young (radiocarbon dating with Radiometric dating is based on the known and constant rate of decay of radioactive isotopes into their radiogenic daughter isotopes.