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Contemporary science issues Lesson 14: Journey to the centre of the Earth © 2006 Gatsby Technical Education Projects.

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Presentation on theme: "Contemporary science issues Lesson 14: Journey to the centre of the Earth © 2006 Gatsby Technical Education Projects."— Presentation transcript:

1 Contemporary science issues Lesson 14: Journey to the centre of the Earth © 2006 Gatsby Technical Education Projects

2 SEISMIC WAVES Can they tell us anything about the Earth’s structure?

3 For each earthquake fact.. Decide whether or not it can help us to build up a model of the Earth’s structure If you think it can, describe what the fact tells us You may want to look at some facts again as you gain more information

4 Waves can change direction when they change speed Example – light can change direction when it enters glass from air and slows down

5 Earthquake waves are like sound waves They travel faster through denser materials Examples: speed of sound in air 330m/s speed in water 1500m/s speed in rock > 5000m/s

6 Scientists know how fast earthquake waves travel but the time they take to reach their destination is longer than it should be if they followed a straight line through the Earth

7 There are 2 types of earthquake waves P-waves (primary or pressure waves) S-waves (secondary or shear waves)

8 P-waves can travel through solids, liquids and gases S-waves can only travel through solids

9 P-waves travel faster than S-waves so reach their destination sooner, but.. S-waves do more damage to buildings

10 P-waves travel as a longitudinal wave; the particles vibrate in the same line as the waves travel Movement of particles wavelength Direction of travel of wave Particles close together Particles far apart

11 S-waves travel as a transverse wave The particles vibrate at right angles to the direction of travel of the wave

12 Earthquake waves follow curved paths through the Earth

13 there is always a region on the opposite side of the Earth from the quake where s-waves cannot be detected P-waves reaching the other side of the world take longer than expected, even when their curving path is accounted for P-waves can be detected nearly all over the world but….

14 epicentre P & S waves detected here No S-waves here: P-waves arrive later than expected No waves at all here

15 The complete picture S-waves stop suddenly here; P-waves change direction suddenly P-waves change direction suddenly again here Both P and S waves follow curving paths here Only P-waves following curving paths here.. …and here

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