Lithosphere 1000 thenosphere P waves 2000 Lower mantie 3000 4000 Outer core 5000 S waves H6000 10 12 14 Velocity (km/sec) Inner core SmartFigure 6.9 hustration showing how P and S wave velocities vary with depth. Although s waves cannot penetrate the outer core, they can still appear in the inner core. When Pwaves strike the bound ary between the inner core and outer core some of that energy is converted into Swaves which then travel though the solid inner core. DELL un adeg
Lithosphere 1000 thenosphere P waves 2000 Lower mantie 3000 4000 Outer core 5000 S waves H6000 10 12 14 Velocity (km/sec) Inner core SmartFigure 6.9 hustration showing how P and S wave velocities vary with depth. Although s waves cannot penetrate the outer core, they can still appear in the inner core. When Pwaves strike the bound ary between the inner core and outer core some of that energy is converted into Swaves which then travel though the solid inner core. DELL un adeg
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
Problem 1LR
Related questions
Question
Based on seismology, why do scientists believe that the density of the Earth’s mantle (the layer shown as red in Figure 6.9) increases as depth increases?

Transcribed Image Text:Depth (km)
Add-ons Help
Last edit was made 7 minutes ago by Aaron Cramer
+ BIUA
Arial
11
GD
Et -E
Lithosphere.
oydsouey
0001
SBABM S
Lower
mantie
0002
000e
Outer
000r
000st
SOMEM S
0009-
9
Velocity (kum/sec)
12
Inner
SmartFigure 6.9 ustration showing how Pand S wave velocities vary with depth. Although S
waves cannot penetrate the outer core, they can still appear in the inner core. When P waves strike the bound-
ary between the inner core and outer core some of that energy is converted into S waves which then travel
though the solid inner core.
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