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Sixth Grade Science Unit 1 Lesson 6
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Seismic Waves are the result of tectonic plate movements under the surface of Earth.
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First there is a disturbance or movement of the plates at the plate boundaries. We call the location of this first disturbance the FOCUS.
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The space between the plate boundaries is called the FAULT.
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The EPICENTER is a point directly above the FOCUS on the surface of Earth. It is used by scientists for measurement purposes.
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Seismic waves are vibrations caused by the energy released in a plate movement event.
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The seismic vibration waves will radiate out from the focus in all directions.
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There are two kinds of Seismic Waves that we are going to study. P waves S waves
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S Wave
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Surface wave Transverse wave Moves perpendicular to its forward motion Will only travel through a solid
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P Wave Compression wave Longitudinal wave Molecules of wave move together and apart as the wave moves forward Wave refracts as it moves through materials with different densities
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P waves travel much faster than S waves and always reach recording stations first.
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S waves P waves
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Wave Movements
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Different Wave Movements
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Shadow Zone is an area where neither P nor S waves go
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To find the exact location of an earthquake, scientists triangulate the data collected at earthquake tracking stations Triangulation of Wave Data
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Circles are drawn around each of three reporting stations at the distance the earthquake was detected. The point at which the three circles Intersect is the EPICENTER. TRIANGULATION
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Parts of a Wave
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More About Waves
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Still More About Waves
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Wave Parts Crest - top of wave Trough – bottom of the wave Wavelength – measurement from one crest to the next Frequency – number of waves that pass a fixed point in a given period of time Amplitude - height of wave from crest to point of equilibrium
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