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A seismologist plots the variation in velocity of P and S waves in different layers of the Earth during an earthquake. The information is shown in the graph.

A seismologist plots the variation in velocity of P and S waves in different layers of the Earth during an earthquake. The information is shown in the graph.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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A seismologist plots the variation in velocity of P and S waves in different layers of the Earth during an earthquake. The information is shown in the graph. 15 P waves 10- S waves 5. Crust Mantle Outer core Inner core 4,000 Depth (km) 5,000 6,000 What can be concluded from the graph? O The layers of Earth have different densities. O Pand S waves are absorbed in the core. O The layers of Earth do not have distinct boundaries. O Pand S waves always originate in the mantle and travel through the core. Activate Wind Go to Settings to a F1 F2 DII ES F4 Prt Scn F6 F7 Home F9 End F10 PgU %23 & Speed (km/s) 各
Transcribed Image Text:A seismologist plots the variation in velocity of P and S waves in different layers of the Earth during an earthquake. The information is shown in the graph. 15 P waves 10- S waves 5. Crust Mantle Outer core Inner core 4,000 Depth (km) 5,000 6,000 What can be concluded from the graph? O The layers of Earth have different densities. O Pand S waves are absorbed in the core. O The layers of Earth do not have distinct boundaries. O Pand S waves always originate in the mantle and travel through the core. Activate Wind Go to Settings to a F1 F2 DII ES F4 Prt Scn F6 F7 Home F9 End F10 PgU %23 & Speed (km/s) 各
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