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Absolute Ages of Rock

Absolute Ages of Rock. Mr. Perez. Important vocabulary. Isotopes Radioactive decay Half-life Radiometric dating Uniformitarianism. Absolute Ages. Absolute age is the age, in years, of a rock or other object. Examples: How old are you? How old is your house? How old is your book bag?

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Absolute Ages of Rock

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  1. Absolute Ages of Rock Mr. Perez

  2. Important vocabulary • Isotopes • Radioactive decay • Half-life • Radiometric dating • Uniformitarianism

  3. Absolute Ages • Absolute age is the age, in years, of a rock or other object. • Examples: • How old are you? • How old is your house? • How old is your book bag? • How old is your pet? • How old is your sibling?

  4. Radioactive Decay • Atoms are made up of: • Nucleus- central region • Includes the protons (+) and neutrons (0) • Electrons- cloud surrounding center (-) • The number of protons(+) determines the identity of the element • The number of neutrons (0) determines the form of the element (aka isotope)

  5. Radioactive Decay • Some isotopes are unstable and break down into other isotopes and particles • We call the above process radioactive decay

  6. Radioactive Decay- Alpha and Beta Decay Both types of decay form a new isotope

  7. Radiometric Decay- Half Life • Each parent isotope decays (breaks down) into its daughter isotope at a certain rate • Based on this decay rate, it takes a certain period of time for one half of the parent isotope to decay to its daughter product • The half-life of an isotope is the time it takes for half of the atoms in the isotope to decay. • Example- It takes carbon-14 5,730 years for half of its atoms to turn into nitrogen-14. Then, it takes another 5,730 years for half of the remaining carbon-14 atoms to turn into nitrogen-14, and so on… THINK OF EXPONENTS! 23 = 8, 32 = 9, 44 = 256

  8. Radioactive Decay- Half-life • Fill in the following table using this information: • Mr. Perez has 100g of carbon-14. After 5,730 years, how many grams of carbon-14 will still be carbon-14? After 2? After 3?...

  9. Radiometric Dating

  10. Radiometric Dating • By measuring the ratio of parent isotope to daughter product in a mineral AND knowing the half-life of the parent, you can calculate the absolute age of a rock • This is called radiometric dating • A scientist must decided which parent isotope to use when measuring the age of a rock. • If it’s old, the scientist will use an isotope with a long half-life • Example: potassium-40 takes 1.25 billion years to decay to argon-40 • To avoid errors, conditions must be met for ratios to give a correct indication of age: • The rock being studied must retain ALL of the argon-40 that produced by the decay of potassium-40 • It cannot contain any contamination of daughter product from other sources

  11. Radiometric Dating- Radiocarbon Dating • Carbon-14 is useful for dating bones, wood and charcoal up to 75,000 years old. • Living things take in carbon from the environment to build their bodies • Most of this carbon is carbon-12, but some is carbon-14 • The radio of these two isotopes is always the same • After an organism dies, the carbon-14 decays slowly • By determining the amounts of isotopes in a sample, scientists can evaluate how much the isotope ratio differs from that in the environment

  12. Radiometric Dating- Radiocarbon Datin

  13. Radiometric Dating- • Age Determinations • Rocks that can be radiometrically dated are mostly IGNEOUS and METAMORPHIC rock • Sedimentary rocks cannot be dated by carbon-14 because they are made up of particles eroded from older rocks • The Oldest Known Rocks • Using radiometric dating, the oldest rocks on Earth are about 3.96 billion years old • The Earth is about 4.5-4.6 billion years old

  14. Uniformitarianism • James Hutton (Scottish scientist in the 1700s) • Estimated that the Earth is much older than we think • Uniformitarianism- principle that states that Earth’s processes occurring today are similar to those that occurred in the past • “The present is the key to the past” • Today, scientists recognize that Earth has been shaped by two types of change • Slow, everyday processes that take place over millions of years • Violent and unusual events

  15. Videos • http://science.howstuffworks.com/environmental/earth/geology/carbon-14.htm • http://teachertube.com/viewVideo.php?video_id=181054&title=Radioactive_decay

  16. Resources • Florida Science Grade 7 Glencoe Science & McGraw Hill Publishing • Google Images

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