Measure isotopes for radiometric dating consolidating contracting microscope

The thing that makes this decay process so valuable for determining the age of an object is that each radioactive isotope decays at its own fixed rate, which is expressed in terms of its half-life.

The methods work because radioactive elements are unstable, and they are always trying to move to a more stable state. This process by which an unstable atomic nucleus loses energy by releasing radiation is called radioactive decay.

When living things die, they stop taking in carbon-14, and the radioactive clock is "set"!

Any dead material incorporated with sedimentary deposits is a possible candidate for carbon-14 dating.

So, we rely on radiometric dating to calculate their ages.

Radiometric dating, or radioactive dating as it is sometimes called, is a method used to date rocks and other objects based on the known decay rate of radioactive isotopes.

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