k Seismic Swave propagation, illustration Seismic Swaves. Cutaway illustration of a section through the Earth, showing seismic waves propagating around the globe. Seismic waves Pwaves and Swaves are waves of energy that travel through the Earths layers as a result of an earthquake, explosion or volcano. Secondary waves Swaves are shear transverse waves which displace the ground perpendicular to the direction of propagation. Swaves are slower than Pwaves primary or pressure waves. They cannot pass through the Earths liquid outer core, and are not detected more than approximately 103 degrees approximately 11,570 kilometres from the epicentre of an earthquake, creating an Swave shadow zone., by SCIENCE PHOTO LIBRARY Stock Photo - Afloimages
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Seismic S wave propagation, illustration Seismic S waves. Cutaway illustration of a section through the Earth, showing seismic waves propagating around the globe. Seismic waves  P waves and S waves  are waves of energy that travel through the Earth s layers as a result of an earthquake, explosion or volcano. Secondary waves  S waves  are shear transverse waves which displace the ground perpendicular to the direction of propagation. S waves are slower than P waves  primary or pressure waves . They cannot pass through the Earth s liquid outer core, and are not detected more than approximately 103 degrees  approximately 11,570 kilometres  from the epicentre of an earthquake, creating an S wave  shadow zone ., by SCIENCE PHOTO LIBRARY
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Seismic S-wave propagation, illustration

Seismic S-waves. Cutaway illustration of a section through the Earth, showing seismic waves propagating around the globe. Seismic waves (P-waves and S-waves) are waves of energy that travel through the Earth's layers as a result of an earthquake, explosion or volcano. Secondary waves (S-waves) are shear transverse waves which displace the ground perpendicular to the direction of propagation. S-waves are slower than P-waves (primary or pressure waves). They cannot pass through the Earth's liquid outer core, and are not detected more than approximately 103 degrees (approximately 11,570 kilometres) from the epicentre of an earthquake, creating an S-wave "shadow zone"., by SCIENCE PHOTO LIBRARY

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