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Potassium-Argon (K-Ar) dating is the most widely applied technique of radiometric dating. Potassium is a component in many common minerals and can be used to determine the ages of igneous and metamorphic rocks. The Potassium-Argon dating method is the measurement of the accumulation of Argon in a mineral.
Radioactive dating is a method that utilizes radioactive elements to calculate the age of geologic materials. Each radioisotope has a unique decay process that occurs at an even and continuous rate. The half-life is the amount of time it takes the parent isotope to decay into atoms of the daughter isotope.
The formula for calculating absolute age of a layer by this method of counting is: Absolute age in years (A) = time elapsed since the formation of the most recent layer (R) plus (the number of layers (N) lying above the layer in question multiplied by the duration (D) of the depositional cycle).
D = D0 + D* Therefore, D = D0 + N (e t 1) or, for small t, D = D0 + N t , This is the basic radioactive decay equation used for determining ages of rocks, minerals and the isotopes themselves.
The amount of Carbon 14 contained in a preserved plant is modeled by the equation f(t) = 10e^{-ct}. Time in this equation is measured in years from the moment when the plant dies (t = 0) and the amount of Carbon 14 remaining in the preserved plant is measured in micrograms (a microgram is one millionth of a gram).
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Among the best-known techniques are radiocarbon dating, potassiumargon dating and uraniumlead dating.
Radiometric Dating. the process of measuring the absolute age of geologic material by measuring the concentrations of radioactive isotopes and their decay products.
Absolute age dating (or, radiometric dating) determines the age of a rock based on how much radioactive material it contains.

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