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Discover the P-wave velocities in Earth's layers, explore seismic results, and find materials with key properties. Uncover insights from seismic tomography and seismic waves. Learn about core composition, mantle dynamics, and crust structures.
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P-wave Velocities Crust 6-7 km/sec Mantle 8-13 km/sec Outer Core 8-10 km/sec Inner Core 10-11 km/sec
K = bulk modulus = resistance of material to squeezing D = density G = shear modulus = resistance of material to shearing
Seismological Results Values of K, G and D at a given point in the Earth’s interior. Search for materials with appropriate values of K, G and D Estimates of composition of different parts of the Earth’s interior
G = 0 for liquids Outer Core of Earth is liquid
From: Understanding Earth by Press, Siever, Grotzinger and Jordan
speed of light in a vacuum = 300,000,000 m/s speed of light in glass = 200,000,000 m/s From: www.what-is-the-speed-of-light.com
Slow Fast Slow Fast
M=7.8, ∆=62° Magnitude 7.8 TARAPACA, CHILE, June 13, 2005 22:45 UTC Boston, Massachusetts - First Wave Arrives 22:55 (10 minutes)
Travel-time versus Distance D Distanced measured in degrees from epicenter.
M=7.6, ∆=97° Magnitude 7.6 PAKISTAN, October 08, 2005 at 03:51 UTC Boston, Massachusetts - First Wave Arrives 4:04 (13 minutes)
M=6.7, ∆=25° Magnitude 6.8 CAYMAN ISLANDS, December 14, 2004 at 23:20 UTC Boston, Massachusetts - First Wave Arrives 23:26 (6 minutes)
Travel Time Distance
1 Path Distance (km) Time (sec) Velocity 1 2,758 360 7.7 km/sec 2 6,563 600 10.9 km/sec 3 9,543 780 12.2 km/sec 2 3 6371 km
P-wave Velocities Crust 6-7 km/sec Mantle 8-13 km/sec Outer Core 8-10 km/sec Inner Core 10-11 km/sec
P-wave Velocities Air: 0.3 Water: 1.4 Concrete: 3.6 Granite: 5.5-6.0 Iron: 5.8 Aluminum: 6.6 Crust 6-7 km/sec Mantle 8-13 km/sec Outer Core 8-10 km/sec Inner Core 10-11 km/sec
Travel-time versus Distance Curves T D Distanced measured in degrees from epicenter. D
Travel-time versus Distance Curves D Distanced measured in degrees from epicenter.
Slow Fast
“Moho” Andrija Mohorovicic Zagreb Seismological Observatory 1909
“Moho” Andrija Mohorovicic Zagreb Seismological Observatory 1909
Fast Slow
Fast Slow
Inner Core discovered by Inge Lehmann in 1936 Copenhagen Seismological Observatory
Inner Core discovered by Inge Lehmann in 1936 Copenhagen Seismological Observatory
Low Velocity Zone in Upper Mantle Low Velocity Zone = Asthenosphere of Plate Tectonics
From Understanding Earth by Press, Siever, Grotzinger and Jordan (2004).
P-wave Velocities Crust 6-7 km/sec Mantle 8-13 km/sec Outer Core 8-10 km/sec Inner Core 10-11 km/sec
Seismic Tomography Variations in seismic velocity (+/- a few percent) are depicted by warm (low velocity) or cool (high velocity) colors.