determine the age of asteroid impact, the isotope of Potassiun, geology homework help
determine the age of asteroid impact, the isotope of Potassiun, geology homework help.
2. In order to determine the age of asteroid impact, the isotope of Potassiun (K-40) was used from the mineral orthoclase. On the space below, draw the radioactive decay graph of K-40 whose specific half-life (SHL) is 1.25 billion years. Indicate the following on the graph:
a. On the x-axis, plot and label 0 to 6 generic half-lives (GHL).
b. On the y-axis, draw and label the parent and daughter radioactive decay curves.
c. The ages of the sample from 0 to 6 generic half-lives using the formula Age = GHL x SHL.
d. Assuming the original amount of parent material is 12,000 grams, calculate the remaining parent material from 0 to 6 GHL.
determine the age of asteroid impact, the isotope of Potassiun, geology homework help
