Unit 5: Geologic Time

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Across
  1. 5. A method of determining the exact age of rocks, fossils, or archaeological artifacts using techniques like radiometric dating, which measures the decay of radioactive isotopes.
  2. 7. The time required for half of a radioactive isotope in a sample to decay into its daughter product.
  3. 10. A gap or break in the geological record where rock layers have been eroded or where deposition was not continuous.
  4. 14. A principle in geology stating that a rock formation or fault that cuts through other layers is younger than the layers it cuts across.
  5. 15. A diagram or visual representation that shows a vertical slice through layers of rock or soil, providing a side view of geological structures.
Down
  1. 1. The stable isotopes or elements formed as a result of the radioactive decay of a parent isotope.
  2. 2. A geological principle stating that in undisturbed rock layers, the oldest layers are at the bottom, and the youngest layers are at the top.
  3. 3. The process by which unstable atomic nuclei lose energy by emitting radiation, transforming into different elements or isotopes.
  4. 4. The vast time scale that represents Earth's history, divided into eons, eras, periods, and epochs.
  5. 6. The original radioactive isotopes that decay into daughter products over time.
  6. 8. The preserved remains, impressions, or traces of once-living organisms, typically found in sedimentary rock.
  7. 9. The permanent disappearance of a species or group of organisms from Earth.
  8. 11. A method of determining the relative order of events or objects without determining their exact age, often using the principles of stratigraphy.
  9. 12. Bodies of igneous rock that form when magma cools and solidifies within preexisting rock layers.
  10. 13. Fossils of organisms that lived during a relatively short, specific time period and are used to help determine the age of rock layers.