Answer:
One half-life
Step-by-step explanation:
The ratio of parent-daughter after one half-life is usually 1:1 and after two half-lives 1/4(0.25) of the parent isotope remains and 3/4(0.75) of the daughter isotope remains and becomes the daughter isotope.
Uranium-238 radioactive properties are used to determine the approximate age of mineral rocks. Uranium-238 (half-life = 4.5 109 years) decays to a stable lead-206 isotope.