Q. ${ }^{238} U$ decays with a half-life of $4.5 \times 10^{9}$ years, the decay series eventually ending at ${ }^{206} Pb$, which is stable. A rock sample analysis shows that the ratio of the number of atoms of ${ }^{206} Pb$ to ${ }^{238} U$ is $0.0058$. Assuming that all the ${ }^{206} Pb$ is produced by the decay of ${ }^{238} U$ and that all other half-lives on the chain are negligible, the age of the rock sample is $\left(\ln 1.0058=5.78 \times 10^{-3}\right.$ )
Nuclei
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