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Absolute Age. Attempts at Absolute Age. Became more important in the age of Darwin. Rate of Sedimentation If the rate was constant over time, then we could tell how old rocks are by their thickness. Radioactivity. Isotopes – elements with different mass number (different number of Neutrons)
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Attempts at Absolute Age • Became more important in the age of Darwin. • Rate of Sedimentation • If the rate was constant over time, then we could tell how old rocks are by their thickness
Radioactivity • Isotopes – elements with different mass number (different number of Neutrons) • These Isotopes break down over time
Radioactive Decay • Release of particles from the nucleus • This decay happens in a predictable way for each element
Rates of Decay • Half Life- time required for half of the radioactive isotope to decay. • Rate of decay are unchanged by environmental conditions • This allows them to be a reliable source for dating
The Rock Clock • Radiometric Dating – use of radioactive decay to date rock ages • Based on the amount of radioactive material left in a rock
The math of radiometric dating What percentage of a radioactive element would you have left after 1 half life? 50% What about 2 half lives? 25% What about 3 half lives? 12.5%