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Unit 6 Geologic Time

Unit 6 Geologic Time. Chapter 21 Fossils and the Rock Record. 21.1 The Rock Record. The geologic time scale - the Earth is 4.6 billion years old. - in order to break up this vast amount of time, scientists divide it into Eons. Eons.

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Unit 6 Geologic Time

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  1. Unit 6 Geologic Time Chapter 21 Fossils and the Rock Record

  2. 21.1 The Rock Record The geologic time scale - the Earth is 4.6 billion years old. - in order to break up this vast amount of time, scientists divide it into Eons

  3. Eons The three earliest eons are grouped into the “Precambrian” Hadean – The formation of the earth 542 Hadean

  4. Eons Archaen – Continental plates begin to form and earliest fossils 542 Hadean

  5. Eons Proterozoic – multicellular life cyanobacteria increases oxygen levels 542 Hadean

  6. Eons Phanerozoic– “visible life” Most of the fossils with hard parts 542 Hadean

  7. Eons are divided into Eras • Phanerozoic is divided into three Eras • Paleozoic – ancient life • Mesozoic – middle life • Cenozoic – recent life 542 Hadean

  8. Eras are divided into Periods • Mesozoic is divided into three Periods • Triassic • Jurassic • Cretaceous 542 Hadean

  9. Periods are divided into Epochs Eons Eras Periods Epochs

  10. If 1 Second was 1 year

  11. You were born 15 seconds ago

  12. If 1 Second was 1 year The Revolutionary War was 4 minutes ago

  13. The First Christmas was 33 minutes ago

  14. The pyramids were built 1.5 hours ago

  15. The Last Ice Age Was 2 hours and 12 minutes ago

  16. Dinosaurs were wiped out 2 years ago

  17. Pangaea broke apart • 6 years and 4 months ago

  18. Dinosaurs showed up (Triassic) • 8 years ago

  19. Cambrian began 17 years ago

  20. Earth formed • 145 years ago

  21. 21.2 Relative-Age Dating • What happened first? • Oldest and newest?

  22. James Hutton • Geologist and Physician • Proposed that the earth was millions of years old based on geologic evidence

  23. Sir Charles Lyell • Geologist • Proposed that geologic changes occur slowly over long periods of time.

  24. Uniformitarianism • The idea that the same processes occurring today have been the same throughout time • This idea replaced the idea of catastophism which suggested major changes by sudden catastrophic events

  25. Principles for Determining Relative Age • Original horizontality – sedimentary rocks are deposited in horizontal layers

  26. Superposition The deeper strata (layers) were deposited first. Fossils found in lower layers are older than in higher layers.

  27. Cross cutting relationships Plutons are younger than the rocks they are found in

  28. Principle of Inclusions Fragments of a rock included in a rock layer are older than the rock layer

  29. Unconformities • Signs of surface erosion that are buried show a gap in the rock record

  30. Disconformities • Signs of surface erosion that are buried between sedimentary layers

  31. Nonconformities • Signs of erosion that are found between a sedimentary layer and metamorphic or igneous layers

  32. Angular Unconformity Nonhorizontal rock layers indicate uplifting

  33. Correlation • Matching of a unique rock layer or fossil in one area to similar layers in another area.

  34. Key Bed A rock layer used as a marker

  35. Fossil Correlation Using index fossils to compare ages of rock layers

  36. 21.3 Absolute-Age Dating So how old is it? Absolute-age dating gives the numerical age of rocks.

  37. Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons

  38. Nucleus C-12

  39. Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons Carbon-14 has 6 protons and 8 neutrons

  40. Nucleus C-14

  41. Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons Carbon-14 has 6 protons and 8 neutrons Carbon-14 decays into Nitrogen-14

  42. Nucleus N-14

  43. Radioactive Decay The decay of radioactive isotopes into the daughter product

  44. Half life The time required for ½ of the isotopes to decay

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