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The Trapped Sea

The Trapped Sea. Jean Nicolet, 1634. The Mediterranean. The Earth’s Plates. Pangaea, 220 m.y. 80 m.y. Plate Tectonics. What Drives It: Convection. What Drives It: Convection. How Plates Move. The Mediterranean Made Simple. The Pieces Today. The Mediterranean, 200 m.y.

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The Trapped Sea

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  1. The Trapped Sea

  2. Jean Nicolet, 1634

  3. The Mediterranean

  4. The Earth’s Plates

  5. Pangaea, 220 m.y.

  6. 80 m.y.

  7. Plate Tectonics

  8. What Drives It: Convection

  9. What Drives It: Convection

  10. How Plates Move

  11. The Mediterranean Made Simple

  12. The Pieces Today

  13. The Mediterranean, 200 m.y.

  14. The Mediterranean, 195 m.y.

  15. The Mediterranean, 175 m.y.

  16. The Mediterranean, 165 m.y.

  17. The Mediterranean, 148 m.y.

  18. The Mediterranean, 123 m.y.

  19. The Mediterranean, 110 m.y.

  20. The Mediterranean, 80 m.y.

  21. The Mediterranean, 63 m.y.

  22. The Mediterranean, 53 m.y.

  23. The Mediterranean, 20 m.y.

  24. The Mediterranean, 15 m.y.

  25. The Mediterranean, 6 m.y.

  26. Filling the Mediterranean National Geographic, January, 1973

  27. The Mediterranean Today

  28. The Aegean

  29. Why Does the Mideast Have So Much Oil?

  30. Africa Closes on Iran

  31. Slab Breaks Arabia Loose

  32. Collision Tilts Arabia

  33. Collision Crumples Crust

  34. Heating Mobilizes Oil

  35. Oil Migrates Into Traps

  36. Good News, Bad News

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