Structure of the Earth (Learning Outcome)

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8 Terms

1
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What are Seismic shadow zones?

They are zone on earth where seismic waves are not detected (no seismic activity is detected)

2
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What did we find out from seismic shadow zones?

Found out that earth had an outer liquid core and a solid inner core

3
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Where are S waves seen?

In the hemisphere where the earthquake occurs

4
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Where can P waves be seen?

They are detected in the hemisphere where the earthquake occurs and on the far side of the planet

5
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Where is the S and P wave shadow zone?

S shadow: It is on the side of the planet that’s opposite to where the earthquake occurs

P shadow: It is the band below mid section of the planet

6
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Describe why there is an S wave shadow zone. What does this reveal about our planet?

This is because S waves are unable to propagate through liquid, therefore, they stop at the core. This reveals that the outer core is liquid

7
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Describe why there is a P wave shadow zone

P waves are able to propagate through a liquid outer core. But when they enter the liquid core they get refracted and bend inwards. They have a lower velocity in liquid outer core than in the mantle. When they exit the liquid outer core, they get refracted again and have P wave energy on the far side of the earth.

8
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What happens if P waves encounter the inner core at a high angle? What does this reveal about our planet? Who discovered this?

The P waves will reflect towards surface of the planet and you can hear very faintly in the shadow zone when they hit the core. This reveals that there is a solid inner core. Inge Lehman who was a woman geoscientist.