Final answer:
The correct statement about nickel-59 is that the amounts of nickel-59 and cobalt-59 in a rock can be used to determine how long ago the rock cooled to the point where those elements were no longer free to move within the rock, a concept known as closure temperature. The correct option is (E).
Step-by-step explanation:
The statement about nickel-59 that is true is:
E. The amounts of nickel-59 and cobalt-59 tell how long ago the rock cooled to closure temperature.
During the decay process, a given quantity of an unstable isotope goes through a well-understood rate of decay described by its half-life.
After one half-life, only half of the original amount of the unstable isotope remains, while the other half has decayed into a more stable form. This is also true for other isotopes used in radioactive dating, such as uranium-238 decaying into lead-206.
For nickel-59 with a half-life of 76,000 years, this does not mean all nickel-59 decays into cobalt-59 in that period, nor does it become stable or maintain equal amounts with cobalt-59 after a single half-life.
Furthermore, rocks can be dated using nickel-59 if they are older than 76,000 years, contrary to what one of the statements suggests.