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Published byEmery Strickland Modified over 6 years ago
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VIRTUAL EARTHQUAKE
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http://www. slideshare
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DIVERGENT BOUNDARY Boundary between two plates that are moving apart.
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CONVECTION CURRENT A current in Earth’s mantle that transfers heat in Earth’s interior and is the driving force for plate tectonics.
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ASTHENOSPHERE Plastic like layer of Earth on which the tectonic plates float and move around.
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LITHOSPHERE The rigid layer of Earth about 100 km thick, made of the crust and a part of the upper mantle.
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CONVERGENT BOUNDARY Boundary where two plates come together. They can form mountain ranges, volcanoes and tranches.
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SEAFLOOR SPREADING When oceanic plates separate and form mid-ocean ridges. Rising magma cools and forms new oceanic crust.
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TRANSFORM BOUNDARY Formed where two plates slide past each other. They move in opposite directions.
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SEISMIC WAVES Waves generated by an earthquake that travel through Earth.
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MAGNITUDE A measure of the energy that is released from an earthquake.
Richter magnitude scale
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TSUNAMI Ocean waves caused by earthquakes. Seismic sea waves.
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VENT An opening in Earth’s surface where magma is released.
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EPICENTER The point on the Earth’s surface directly above the focus of the earthquake.
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FOCUS The point where the energy release of the earthquake first occurs. Located about 65 km beneath the surface of the Earth.
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SEISMOGRAPH An instrument that measures seismic waves from earthquakes and volcanic eruptions. They register the waves and record the time of the wave arriving at the station.
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PRIMARY WAVES Particles in rock stretch and compress as energy moves through it. The first wave that leaves the focus of the earthquake.
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SECONDARY WAVES Particles in rock move in a backward, rolling motion and a side to side, swaying motion. Picture a wave moving through a jump rope.
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