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Lutetium 176 dating technique

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Radiometric dating The process of determining the age of rocks from the decay of their radioactive elements has been in widespread use for over half a century [1].

There are over forty such techniques, each using a different radioactive element or a different way of measuring them.

Lutetium is the heaviest and hardest of the rare earth elements.

Lutetium has the highest melting point of any lanthanide, probably related to the lanthanide contraction.

It has become increasingly clear that these radiometric dating techniques agree with each other and as a whole, present a coherent picture in which the earth was created billions of years ago.

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These radioactive elements constitute independent clocks that allow geologists to determine the age of the rocks in which they occur.

A strict correlation between periodic table blocks and chemical series for neutral atoms would describe lutetium as a transition metal because it is in the d-block, but it is a lanthanide according to IUPAC.

Lutetium is a silvery white corrosion-resistant trivalent metal that is relatively stable in air.

Most do not realize the scientific community is rather unified on the earth being several billion years in age.

The most straightforward dating technique is emphasized in this paper – radiometric dating.