Potassium-40 (40K) is a radioactive material that decays into argon-40 (40Ar). The half-life of a sample of 40K is 1.3 billion years. Rocks containing 40K have been around since the formation of the earth, and 40Ar gas has been accumulating in those rocks since the earth formed. However, when rocks are heated by volcanic action, all the 40Ar leaves the rock when the gases escape. Create a scenario and discuss, based on your knowledge of half-life, the value of potassium-argon dating to geologists.
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Knowing the half life of K-40, the ratio of Ar-40 : K-40 in a sample of volcanic rock can be used to determine when the volcanic eruption took place. Knowing when the eruption took place is useful to volcanologists and geologists in studying things such as plate tectonics.
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