Final answer:
The age of the rock from which the sample was taken is approximately 150 million years, calculated by multiplying the number of half-lives (3) needed to reduce the isotope sample to 1/8 its original amount by the half-life duration (50 million years).
Step-by-step explanation:
If an isotope has a half-life of 50 million years, and 1/8 of the original sample remains, we can determine the age of the rock by considering how many half-lives have passed. After one half-life, half of the original isotope remains (1/2), after two half-lives, a quarter remains (1/4), and this process continues such that after three half-lives, an eighth remains (1/8).
Since each half-life is 50 million years and we need 3 half-lives for the sample to be reduced to 1/8, we multiply the number of half-lives by the length of one half-life:
3 half-lives × 50 million years/half-life = 150 million years
Therefore, the rock is approximately 150 million years old.