6. 1.2 (Mantie)
F
F
2,000
F F F
1.3 F
1.) F (Outer Core) F
F
2.) F (Inter Core) F
F
7. 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 F
F F (Laurasia) F F F
(Gond-wanaland)
F 60 F F F
F
8. F F FF
F F F F F F F
F
F
F F 1-10 F F
F F
F F F F
F F
9. 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
F
3.2 F
F F 2 F F F
F F F F (Oceanic Plate) F
F F (Continental Plate) F
F3
10. F
F (plates)
F F
F F F F
F F 200 F
F F " " (Pangaea)
F
F F
F F F F
F F
F F F F F
F (plate tectonices)
18. 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
19. 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 F
F 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
20. 2. (Fault) F
F F F F
F F
2.1) Normal Fault F
F F F F Downthrow
F
24. 1. F
F (Earthquake) F
F F F F F F
F
1.1 F F
F F F F F F
F F F F F
90 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
25.
26. F F F F
F F F
F 5 F F (After
Shock) 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
27. 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 1,000
3.) (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
28. 1.3 F
1.) F F
F F F F F
F F F
F F F F F
F F F
F
1.4 F
F F F
F F F
F F F F F
F F F
F F F F
F F F F F