1. FAULTS

2. WHAT IS THIS?

3. WHO WILL WIN THIS? ROUND 1

4. THE SECOND BEST ROUND

5. THE SECOND BEST TEST RUN SCORER

6. THE SECOND BEST GOOGLE INDIAN 2011

7. THE SECOND BEST TAMIL MOVIE GROSSER

8. THE SECOND PRIME MINISTER OF INDIA

9. THE SECOND MAN TO SET FOOT ON MOON

10. THE SECOND MOST IMPORTANT REASON FOR
EARTHQUAKES
 TECTONIC PLATES

11. A MATTER OF DEPTH

12. FAULTS
 FAULTS ARE ONE OF THE STRUCTURAL
FEATURES OF ROCKS
 WHILE ROCKS AT OR NEAR THE
SURFACE OF THE EARTH ARE COOL &
BRITTLE, ROCKS BELOW THE SURFACE
OF THE EARTH ARE HOT AND TEND TO
MOVE

13. FAULTS
 A LOT OF EXTERNAL FORCES ACT UPON
THE ROCKS AND CAUSE STRESS ON THEM
 DUE TO THIS STRESSES, ROCKS EITHER
UNDERGO DUCTILE DEFORMATION OR
BRITTLE DEFORMATION
 IF THEY UNDERGO DUCTILE
DEFORMATION, ROCKS DEVELOP FOLDS.
IF THEY UNDERGO BRITTLE
DEFORMATION, THEY DEVELOP FAULTS.

14. FAULTS
 FAULT IS DEFINED AS A SPLIT OR CRACK
OR FRACRTURE IN THE ROCK PRESENT
IN EARTH’S CRUST CHARACTERISED BY
RELATIVE DISPLACEMENT OF ONE SIDE
OVER THE OTHER.

15. FAULTS

16. FAULTS

17. FAULT LINE
 A FAULT LINE IS THE INTERSECTION OF
A FAULT PLANE AND EARTH SURFACE
 IT IS THE SURFACE TRACE OF A FAULT

18. FAULTS

19. FAULTS

20. TYPES OF FAULTS
 FAULTS ARE CLASSIFIED INTO THREE
TYPES NAMELY
 DIP SLIP FAULTS (VERTICAL MOTION)
 STRIKE SLIP FAULTS (HORIZONTAL
MOTION)
 OBLIQUE SLIP FAULTS (OBLIQUE
MOTION)

21. TYPES OF FAULTS

22. DIP SLIP FAULTS
 Normal Faults (Extension)
 Reverse Faults/Thrust Faults (Compression)

23. NORMAL FAULTS

24. REVERSE FAULTS

25. STRIKE SLIP FAULTS
 Left Lateral
 Right Lateral

26. LEFT LATERAL FAULTS

27. RIGHT LATERAL FAULTS

28. OBLIQUE SLIP FAULTS

29. SIMPLE DIAGRAMATIC REPRESENTATIONS

30. SYMBOLS FOR FAULTS

31. FAULTS & EARTHQUAKES
FAULTS CAN CAUSE TREMENDOUS
EARTHQUAKES
THE ORDER OF CAUSE AND IMPACT OF
EARTHQUAKES
STRIKE SLIP
OBLIQUE SLIP
DIP SLIP

32. FAULTS & EARTHQUAKES

33. ELASTIC REBOUND THEORY

34. ELASTIC REBOUND THEORY

35. ELASTIC REBOUND THEORY

36. ELASTIC REBOUND THEORY
 The elastic rebound theory is an explanation
for how energy is spread during earthquakes.
As plates on opposite sides of a fault are
subjected to force and shift, they accumulate
energy and slowly deform until their internal
strength is exceeded. At that time, a sudden
movement occurs along the fault, releasing
the accumulated energy, and the rocks snap
back to their original undeformed shape.