# K–Ar dating facts for kids

**Potassium–Argon dating** or **K–Ar dating** is a radiometric dating method used in geochronology and archaeology. It is based on measurement of the product of the radioactive decay of an isotope of potassium (K) into argon (Ar).

Potassium is a common element found in many materials, such as micas, clay, tephra, and evaporites. In these materials, the decay product ^{40}Ar is able to escape the liquid (molten) rock, but starts to build up when the rock solidifies (recrystallises). Time since recrystallization is calculated by measuring the ratio of the amount of ^{40}Ar to the amount of ^{40}K remaining. The long half-life of ^{40}K is more than a billion years, so the method is used to calculate the absolute age of samples older than a few thousand years.

Quickly cooled lavas make nearly ideal samples for K–Ar dating. They also preserve a record of the direction and intensity of the local magnetic field at that time. The geomagnetic polarity time scale was calibrated largely using K–Ar dating.

## See also

In Spanish: Datación potasio-argón para niños

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