Dating is very important in any aspect of human interest. Wherever we go, whatever we encounter, we are required the age or be able to answer the question; how old it is? In the vast field of archaeology, determining the age of any object is very crucial and difficult. The analysis will be absolutely wrong and far away from the reality. We will loose an important key or part of the puzzle, which can never be recovered.
Argon Geochronology for the Earth Sciences (AGES) Lab
The potassium-argon K-Ar isotopic dating method is especially useful for determining the age of lavas. Developed in the s, it was important in developing the theory of plate tectonics and in calibrating the geologic time scale. Potassium occurs in two stable isotopes 41 K and 39 K and one radioactive isotope 40 K. Potassium decays with a half-life of million years, meaning that half of the 40 K atoms are gone after that span of time.
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The Reston Groundwater Dating Laboratory
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