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Time since recrystallization is calculated by measuring the ratio of the amount of The quickly cooled lavas that make nearly ideal samples for K–Ar dating also preserve a record of the direction and intensity of the local magnetic field as the sample cooled past the Curie temperature of iron.

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K–Ar dating was instrumental in the development of the geomagnetic polarity time scale.

Although it finds the most utility in geological applications, it plays an important role in archaeology.

The ratio of the amount of K which was present at the beginning of the elapsed time period.

In practice, each of these values may be expressed as a proportion of the total potassium present, as only relative, not absolute, quantities are required.

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