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Published byMelvin Banks Modified over 9 years ago
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Earthquakes Earth shaking
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Basic Earthquake Words: The epicenter and focus Force pushing Force pushing Fault is a crack That forms Along the break An Earthquake is the group of waves that spread away from the focus
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Earthquakes require a brittle-solid that breaks – the lithosphere - force builds but no shape changing shape, not plastic - break/shatters when force large enough - Earth material (rock) goes twang, energy released as earthquake waves Lithosphere: (plate) brittle solid, strong earthquakes Mantle: plastic – oozes Outer Core: liquid Inner Core: solid
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Earthquakes are concentrated around plate boundaries Depth of Focus: 0-70 km 70-300 km 300-700 km Plates
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(Garrison, 1993) Pressure, Primary (P) waves: - squeeze - slinky push-pull - faster than sideways wave in Earth - travels through solids and liquids - Ex: sound only pressure wave Sideways, Secondary (S) waves: - rope wiggle - slower than pressure wave in Earth - travels through solids, NOT liquids Solids transmit P and S waves - Sudden force in a solid makes P and S together, usually cannot separate - Example: smack board with hammer Earthquakes Exist In the Form of Waves: Most expressed are P & S
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Actually, there are three types of Earthquake waves P=Pressure wave Slinky push-pull, Caterpillar scrunch Fastest, 1 st to arrive S=Shear wave Sideways wiggle Slinky sideways wiggle Rope wiggle Slower, 2 nd to arrive Surface Wave Only travels on a surface, Maximum movement on surface, Movement decreases away from surface, Movement disappears far enough away from surface Slowest, 3 rd to arrive Causes Most of the Damage 2 Flavors Of Surface waves
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An earthquake in lithosphere (plate) makes P, S and Surface waves that spread outward in all directions If the Earth were uniform, stronger P and S waves would travel inside in straight lines through the entire Earth. = focus Surface Waves Only travel On the surface
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Seismometer Recording of an Earthquake: A record of the winners of a race with P arriving first, S second, Surface last
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P & S waves inside the Earth - do not travel in straight lines - take different routes Can’t Be Observed Explanation requires A Non-uniform Earth
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The San Andreas Fault: Our nearest plate boundary
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Lakes. <>
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Japan’s Earthquakes
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The End
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