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Earth Portrait of a Planet Chapter 10 Earthquake

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Presentation on theme: "Earth Portrait of a Planet Chapter 10 Earthquake"— Presentation transcript:

1 Earth Portrait of a Planet Chapter 10 Earthquake

2 Fig U.S. Geological Survey

3 Fig W. W. Norton

4 J. Dewey, U.S. Geological Survey
Fig J. Dewey, U.S. Geological Survey

5 Fig lle W. W. Norton

6 Fig n) shear) W. W. Norton

7 Types of Faults This animation shows the differences between the three types of faults and illustrates how they are formed. View 1 shows a normal fault, View 2 shows a reverse fault, and View 3 shows a strike-slip fault. [by Stephen Marshak] Play Animation Windows version >> Play Animation Macintosh version >>

8 National Geophysical Data Center/NOAA W. W. Norton
Fig National Geophysical Data Center/NOAA W. W. Norton

9 Fig a-f W. W. Norton

10 Photo courtesy of Paul “Kip” Otis-Diehl, USMC, 29 Palms, CA
Fig g Photo courtesy of Paul “Kip” Otis-Diehl, USMC, 29 Palms, CA

11 Fig W. W. Norton

12 Fig W. W. Norton

13 Fig W. W. Norton

14 Fig W. W. Norton

15 Original artwork by Gary Hincks
p a Original artwork by Gary Hincks

16 Original artwork by Gary Hincks
p b Original artwork by Gary Hincks

17 Fig W. W. Norton

18 Fig W. W. Norton

19 Fig ab W. W. Norton

20 Fig cd W. W. Norton

21 Fig ef W. W. Norton

22 Seismic Wave Motion Seismologists distinguish between different types of seismic waves based on how they move, and whether they travel along the Earth's surface (surface waves) or pass through its interior (body waves). This animation shows two types of body wave motion: View 1 shows shear body waves (also called S-waves) and View 2 shows compressional body waves (P-waves). [by Stephen Marshak] Play Animation Windows version >> Play Animation Macintosh version >>

23 Fig W. W. Norton

24 Fig W. W. Norton

25 How a Seismograph Works
Seismologists use two basic configurations of seismographs, one for measuring horizontal ground motion, like the one shown in this animation, and the other for measuring vertical ground motion. Both work on the principle of inertia as described by Newton's law, which states that an object at rest tends to remain at rest unless acted on by an outside force. Thus, during an earthquake, vibrations cause the frame of the seismograph to move. The pendulum apparatus remains fixed as the paper cylinder moves back and forth beneath it. [by Stephen Marshak] Play Animation Windows version >> Play Animation Macintosh version >>

26 Fig W. W. Norton

27 Fig W. W. Norton

28 Fig ab W. W. Norton

29 Fig c W. W. Norton

30 Fig W. W. Norton

31 W. W. Norton. Adapted from Bolt, 1978.
Fig W. W. Norton. Adapted from Bolt, 1978.

32 W. W. Norton. Modified from Dolgoff, 1996.
Fig W. W. Norton. Modified from Dolgoff, 1996.

33 Fig W. W. Norton

34 Fig W. W. Norton

35 Fig W. W. Norton

36 W. W. Norton. Adapted from U.S. Geological Survey.
Fig a W. W. Norton. Adapted from U.S. Geological Survey.

37 Fig W. W. Norton

38 Fig ab W. W. Norton

39 Fig cd W. W. Norton

40 Fig e W. W. Norton

41 Fig fg W. W. Norton

42 M. Celebi, U.S. Geological Survey
Fig b M. Celebi, U.S. Geological Survey

43 J. Dewey, U.S. Geological Survey
Fig c J. Dewey, U.S. Geological Survey

44 Fig ab W. W. Norton

45 National Geophysical Data Center/NOAA
Fig c National Geophysical Data Center/NOAA

46 Fig W. W. Norton

47 Fig b U.S. Geological Survey

48 Fig W. W. Norton

49 Cecilio Licos, Yasuki Arakaki Collection/Pacific Tsunami Museum
Fig a Cecilio Licos, Yasuki Arakaki Collection/Pacific Tsunami Museum

50 Pacific Tsunami Museum
Fig b Pacific Tsunami Museum

51 Fig c NOAA

52 Fig a W. W. Norton

53 Fig bc W. W. Norton

54 Fig d W. W. Norton

55 Fig a W. W. Norton

56 Fig b W. W. Norton

57 Fig c W. W. Norton

58 Fig W. W. Norton

59 Adapted from Wesson and Wallace, 1985.
Fig abc Adapted from Wesson and Wallace, 1985.

60 Adapted from Wesson and Wallace, 1985.
Fig d Adapted from Wesson and Wallace, 1985.

61 Adapted from Nishenko, 1989 (U.S. Geological Survey).
Fig a Adapted from Nishenko, 1989 (U.S. Geological Survey).


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