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1 โลกและการเปลี่ยนแปลง

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1 โลกและการเปลี่ยนแปลง

  1. 1. 1 2 F
  2. 2. 1. F1.1 (Crust) 6-70 FF F F F F F F F F F F F F 2
  3. 3. 1 F F F F F F 2 F FF F F F F F F
  4. 4. 1.2 (Mantie) F F 2,000 F F F1.3 F 1.) F (Outer Core) F F 2.) F (Inter Core) F F
  5. 5. 2. F F F F F F F F (Theory of Continnentai) . . 2455 F F F 200 F F F FF F F (Pangea) F F F (Panthalassa) F 140 F F F FF F (Laurasia) F F F (Gond-wanaland) F 60 F F F F
  6. 6. F F FF F F F F F F FF F F F 1-10 F F F F F F F F F F
  7. 7. 3. F FF F F F F F F F F F (Jigsaw) F F F F F (Tectonic plate)3.1 F F F F F F F3.2 F F F 2 F F F F F F F (Oceanic Plate) F F F (Continental Plate) F F3
  8. 8. F F (plates) F F F F F F F F 200 F F F " " (Pangaea) FF F F F F F F F F F F F F F (plate tectonices)
  9. 9. 200 F 60 F F
  10. 10. F
  11. 11. 1. F F (Divergent Boundary) F F F 2 F F F F F F F F2. F F (ConvergentBoundary) 3
  12. 12. 2.1) F F 2 F (Collision) F F F FF F F F
  13. 13. 2.2) F F F FF F F F F F
  14. 14. 2.3) F F 40 F F F - F F F FF F F F
  15. 15. 3. F F (Transform Boundary)F F F F F F F
  16. 16. 3. F F F F F F F F (Fold) (Fault) F 1. F (Fold) F 2 F F F F F F F F F F F F
  17. 17. 1.1) F (Simple Fold) F F 2 F F 1.2) F F (Asymmetrical Fold or Inclined Fold) F 2 F F F F F F 1.3) F F F F FF F F F F F 1.4) F F F F F F F F F 1.5) F F F F F F F
  18. 18. 2. (Fault) F F F F F F F 2.1) Normal Fault F F F F F DownthrowF
  19. 19. 2.2) Reverse Fault F 2F F F
  20. 20. 2.3) Tear Fault F 2 F F FF F
  21. 21. 1. F F (Earthquake) F F F F F F F F1.1 F F F F F F F F F F F F F90 F F F F (The Ring of Fire) F F F F F F (Focus Hypocenter) F F F F F F F F (Epicenter) F F
  22. 22. F F F F F F F F 5 F F (AfterShock) F F F 2 P (Primary) S(Secondary)( P F S)1.2 F 1.) F (Focal Depth) F 1.1) F (Shallow Earthquake) F F F 0-70 1.2) F (Intermediate Earthquake) F F F 70-300 1.3) F (Deep Earthquake) F F F 300-700
  23. 23. 2.) F F F F (Epicenter) F 2.1) F F (Shallow Earthquake) F F 100 2.2) F F (Shallow Earthquake) F F 100-1,000 2.3) F (Teleseism Earthquake) F 1,0003.) (Magnitude) F 3.1) F F (Micro Earthquake) F F 2 F 3.2) F (Micro Earthquake) 3-4 F 3.3) F (Micro Earthquake) 4-5 F 3.4) F (Micro Earthquake) F 6 F
  24. 24. 1.3 F 1.) F F F F F F F F F F F F F F F F F F F1.4 F F F F F F F F F F F F F F F F F F F F F F F F
  25. 25. F
  26. 26. 1.5 F F (Magnitude) F F F F F F F (Amplitude) F F F F F . . F (C.F.Richter) F F F F F F F F F F F F F
  27. 27. F F2 F F F F1 F F F F F F F2 F F 8 F F F F3 F F F F F4 F F F F 9 F F F F F F F F F5 10 F F F F F F F F6 F F F 11 F F7 F F 12 F F F
  28. 28. F (Intensity) F F F F F F F F F F F F F1.6 F F F F F F F F F F F F F F
  29. 29. 1.7 F F F F F F F F F FF F 1.) 1. 2. F 3. F 4. F 5. F
  30. 30. 2.) F 1. F F 2. F 3. 4. 3.) F F FF F F F F F
  31. 31. 2. F F F F F F FF (Lava) FF F
  32. 32. 2.1 F FF F F F F F FF F F F F (Ring of Fire)
  33. 33. 2.2 F F F4 F 1.) (Steep Cone) 1. 2. 3. F F F F F F F 4. F F F
  34. 34. 2.) F (Shield Volcano) 1. 2. F F F FF F 3. F F F F F F F
  35. 35. 3.) (Ash and Cinder Cone) 1. F 2. F F FF 3. F F F
  36. 36. 4.) (Composite Cone) 1. F (Symmetry) F F F 2. F FF F F F 3. F F F F F 4. F F F F
  37. 37. 2.3 F F F F F F F F F (Cone) F F F F (Crater) F F F F F F F(Crater Lake)
  38. 38. 2.4 F F F F F2 3 F 5,000 55 F F FF F F F F F F F F F FF F F 3
  39. 39. 1.) F F (Active) F F 2.) (Dormant) 3.) F (Extinct) F F F F F F F F F F F 2.5 F F F F F FF F F F F
  40. 40. F 1. F F F 2. F F F 3. F F F F F 4. F 1. F F F 2. F F F F F FF F F

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