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GEOLOGIC TIME

GEOLOGIC TIME. Rocks Record Earth History. Discovering Earth’s History .  Rocks record geological events and changing life forms of the past.

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GEOLOGIC TIME

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  1. GEOLOGIC TIME

  2. Rocks Record Earth History Discovering Earth’s History  Rocks record geological events and changing life forms of the past. We have learned that Earth is much older than anyone had previously imagined and that its surface and interior have been changed by the same geological processes that continue today.

  3. A Brief History of Geology Discovering Earth’s History  Uniformitarianism means that the forces and processes that we observe today have been at work for a very long time.

  4. Relative Dating—Key Principles Discovering Earth’s History  Relative datingtells us the sequence in which events occurred, not how long ago they occurred.  Law of Superposition The law of superposition states that in an undeformed sequence of sedimentary rocks, each bed is older than the one above it and younger than the one below it.

  5. Ordering the Grand Canyon’s History

  6. Relative Dating—Key Principles Discovering Earth’s History  Principle of Original Horizontality The principle of original horizontality means that layers of sediment are generally deposited in a horizontal position.

  7. Disturbed Rock Layers

  8. Relative Dating—Key Principles Discovering Earth’s History  Principle of Cross-Cutting Relationships The principle of cross-cutting relationships states that when a fault cuts through rock layers, or when magma intrudes other rocks and crystallizes, we can assume that the fault or intrusion is younger than the rocks affected.

  9. Applying Cross-Cutting Relationships

  10. Relative Dating—Key Principles Discovering Earth’s History  Unconformities An unconformity represents a long period during which deposition stopped, erosion removed previously formed rocks, and then deposition resumed. It shows a gap in the rock record.

  11. Discovering Earth’s History http://www.classzone.com/books/earth_science/terc/content/visualizations/es2902/es2902page01.cfm?chapter_no=visualization http://www.youtube.com/watch?v=OszS0fblz6o (geologize)

  12. Fossils and Correlation Fossils: Evidence of Past Life  The principle of fossil succession states that fossil organisms succeed one another in a definite and determinable order. Therefore, any time period can be recognized by its fossil content. • Index fossilsare widespread geographically, are limited to a short span of geologic time, and occur in largenumbers.Ammonite- found in Mesozoic, • but not after the Cretaceous • graptolite- good for dating Paleozoic

  13. graptolites, gingko, trilobite Fossil Formation Fossils: Evidence of Past Life  Interpreting Environments • Fossils can also be used to interpret and describe ancient environments.

  14. Fossil Formation Fossils: Evidence of Past Life  Altered Remains • The remains of an organism are likely to be changed over time. • Fossils often become petrified or turned to stone. • Molds and casts are another common type of fossil. • Carbonization is particularly effective in preserving leaves and delicate animals. It occurs when an organism is buried under fine sediment. Video on fossils

  15. Fossil Formation Fossils: Evidence of Past Life  Indirect Evidence Trace fossils are indirect evidence of prehistoric life. Examples are tracks, trails, nests, bite marks, burrows, borings and coprolites.  Conditions Favoring Preservation Two conditions are important for preservation: rapid burial and the possession of hard parts.

  16. Overlapping Ranges of Fossils

  17. Radiometric Dating Dating with Radioactivity  Each radioactive isotope has been decaying at a constant rate since the formation of the rock in which it occurs.  Radiometric dating is the procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes.

  18. Radiometric Dating Dating with Radioactivity  As a radioactive isotope decays, atoms of the daughter product are formed and accumulate.  An accurate radiometric date can be obtained only if the mineral remained in a closed system during the entire period since its formation.

  19. Radioactive Isotopes Frequently Used in Radiometric Dating

  20. Dating with Carbon-14 Dating with Radioactivity  Radiocarbon dating is the method for determining age by comparing the amount of carbon-14 to the amount of carbon-12 in a sample.  When an organism dies, the amount of carbon-14 it contains gradually decreases as it decays. By comparing the ratio of carbon-14 to carbon-12 in a sample, radiocarbon dates can be determined.

  21. Structure of the Time Scale The Geologic Time Scale  Based on their interpretations of the rock record, geologists have divided Earth’s 4.56-billion-year history into units that represent specific amounts of time. Taken together, these time spans make up the geologic time scale.

  22. Structure of the Time Scale The Geologic Time Scale  Eonsrepresent the greatest expanses of time. Eons are divided into eras. Each era is subdivided into periods. Finally, periods are divided into smaller units called epochs.  There are three eras within the Phanerozoic Eon: the Paleozoic, which means “ancient life,” the Mesozoic, which means “middle life,” and the Cenozoic, which means “recent life.”

  23. Structure of the Time Scale The Geologic Time Scale  Each period within an era is characterized by somewhat less profound changes in life forms as compared with the changes that occur during an era.  The periods of the Cenozoic era are divided into still smaller units called epochs, during which even less profound changes in life forms occur.

  24. Precambrian Time The Geologic Time Scale  During Precambrian time, there were fewer life forms. These life forms are more difficult to identify and the rocks have been disturbed often.

  25. Be ready to discuss these questions in class • What is the difference between relative dating and absolute dating? • Why are fossils found only in sedimentary rocks? • List the 3 eras in the Phanerozoic Eon from oldest to youngest. • What saying could you use to remember the order of the periods of the Paleozoic Period? • In what era did dinosaurs dominate? • In what era/period/epoch are we in today?

  26. 7. What 2 conditions are necessary to preserve organisms? 8. Why can carbon dating only be used with organisms that have died less than 60,000 years ago? 9. What is the stable isotope into which C-14 decays? 10. Where do plants get C-14? Where do consumers get the C-14? 11. Give 3 examples of trace fossils. Did you know what a coprolite was or did you look it up? Always look up words you don’t know!

  27. 12. A. List the 3 oldest rocks from oldest to youngest.B. What law did you use to date these layers? C. What can you say about the relative ages of rocks C and A? Rocks E and A? D. What is the name of a feature such as A that cuts through other rock?

  28. Q: Where do geologists like to relax?A: In a rocking chair!

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