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PLATE TECTONICS A PRIMER
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PLATE TECTONICS Heat flowing from the interior of the earth through the mantle and lithosphere to the surface is the engine that causes major and minor portions of the Earth’s crust (i.e., tectonic plates) to slowly converge, diverge, or slide past each other over time. The relative movement of plates causes compression, tension, or shear, which causes faulting and earthquakes.
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HEAT FLOW IS GREATER AT PLATE BOUNDARIES
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TECTONIC PLATES TWO EARTH DAYS AGO
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TECTONIC PLATES TODAY
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PLATE TECTONICS Plate boundaries are defined by seismic activity (i.e., seismicity) . Plate boundaries are often marked by prominent fault zones that may in some cases cause notable surface faulting.
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Plate Movement Causes Three Primary Kinds Of Faulting
Strike-Slip Reverse Three types of faults Form depending on type of plate motion and complex reaction of earth’s lithospheric blocks Strike-slip Normal Thrust Normal
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EARTHQUAKES DEFINE PLATE BOUNDARIES: PACIFIC, EURASIAN, NA, SA, NASCA, CARIBBEAN, COCOS, AND PHILIPPINES PLATES
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SOME CONVERGING PLATES UNDERGO SUBDUCTION AND CAUSE VOLCANOES
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FAULT BOUNDARIES: CASCADIA, NORTH AMERICA, AND PACIFIC PLATES
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JUAN DE FUCA PLATE IS SUBDUCTING BENEATH NORTH AMERICAN PLATE
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COCOS PLATE IS SUBDUCTING BENEATH NORTH AMERICAN PLATE
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MOTAGUA FAULT:1976 GUATEMALA QUAKE
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SAN ANDREAS FAULT: PACIFIC AND NORTH AMERICAN PLATE BOUNDARY
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1,000-KM-LONG SAN ANDREAS FAULT SYSTEM
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SURFACE FAULT RUPTURE: 1906 SAN FRANCISCO QUAKE
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Schematic Diagram of the Earthquake Mechanism
WEST NORTH
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Schematic Diagram of the Strike-Slip Earthquake Mechanism: 1989 Loma Prieta, CA
WEST NORTH
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ARABIAN, AFRICAN, ANATOLIAN, INDIAN, AND EURASIAN PLATES
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DEAD SEA RIFT: BOUNDARY OF ARABIAN AND AFRICAN PLATES
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NORTH ANATOLIAN FAULT: EURASIAN AND ARABIAN PLATES
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NORTH ANATOLIAN FAULT: 1999 KOCALEI, TURKEY QUAKE
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NORTH ANATOLIAN SURFACE FAULTING: 1999 KOCALEI QUAKE
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SOME CONVERGING PLATES CAUSE COLLISION AND MOUNTAIN BUILDING
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COLLISION OF INDO-AUSTRALIAN AND EURASIAN PLATES
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250-KM-LONG LONGMENSHAN FAULT ZONE: CHINA QUAKE OF MAY 12, 2008
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250-KM-LONG LONGMENSHAN FAULT ZONE: CHINA QUAKE OF MAY 12, 2008
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PAKISTAN EARTHQUAKE: OCTOBER 8, 2005
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