Suggest — 2 marks
A seismic monitoring station detects vibrations from an earthquake. The station records both P-waves (primary waves) and S-waves (secondary waves) arriving at different times. P-waves travel through both solid rock and liquid magma in the Earth's interior, whereas S-waves only travel through solid rock. Scientists use the time difference between the arrival of these two wave types to locate the earthquake's epicentre and determine the structure of the Earth's interior.
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Suggest why S-waves cannot travel through the liquid outer core of the Earth, whereas P-waves can.
[1 mark]
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Suggest one reason why the time difference between P-wave and S-wave arrival times increases with greater distance from the earthquake epicentre.
[1 mark]
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Explain — 2 marks
A geologist uses seismic waves to investigate the structure of the Earth after an earthquake. Two types of waves are detected: primary waves (P-waves) that travel through both solids and liquids, and secondary waves (S-waves) that only travel through solids. The S-waves cannot pass through the Earth's liquid outer core, creating a 'shadow zone' where they are not detected.
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Explain why S-waves cannot travel through the liquid outer core of the Earth.
[1 mark]
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Explain why P-waves are able to travel through both the solid mantle and the liquid outer core.
[1 mark]
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