Crew Severin - Layers of the Earth and Plate Tectonics

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Across
  1. 1. The process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary
  2. 3. A dropped zone where the plates are pulling apart
  3. 4. Layer of the crust that is broken up into tectonic plates
  4. 5. Theory created by Alfred Wegner that states that all 8 continents (including India) were once connected in one large supercontinent
  5. 6. Type of rock that continental plates are made from
  6. 8. An arch shaped chain of volcanoes formed above a subduction zone
  7. 11. A molten mixture of rock-forming substances, gases, and water from the mantle
  8. 16. A dense sphere of solid iron and nickel at the center of Earth
  9. 17. The process by which molten material adds new oceanic crust to the ocean floor
  10. 20. A plate boundary where two plate move toward each other
  11. 21. A layer of molten iron and nickel that surrounds the inner core of Earth
  12. 22. An undersea valley that represents one of the deepest parts of the ocean
  13. 23. The study of Earth's magnetic polarity, as recorded in rocks that are high in iron
  14. 24. The layer of rock that forms Earth's outer surface
Down
  1. 1. Vibrations that travel through Earth carrying the energy released during an earthquake
  2. 2. An undersea mountain chain where new ocean floor is produced; a divergent boundary plate boundary under the ocean
  3. 7. A plate boundary where two plates move past each other in opposite directions
  4. 9. Force that drives the movement of tectonic plates on Earth
  5. 10. The layer of hot, solid material between Earth's crust and core
  6. 12. The shaking that results from the movement of rock beneath Earth's surface
  7. 13. The phenomenon where Earth's magnetic field flips
  8. 14. The type of rock that oceanic plates are made from
  9. 15. A plate boundary where two plate move away from each other
  10. 18. The slowly moving, semi-molten layer of the upper mantle
  11. 19. Scientist who developed the theory of Continental Drift