Faults - Movements that produce earthquakes are usually associated with large fractures in Earth's crust called faults Most of the motion along faults can be explained by plate tectonics
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Slippage along Faults
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Types of Faults There are three major types of
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How do Faults cause Earthquakes?
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Principle of the Seismograph
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Seismology: Seismographs
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Seismology: Body Wave Motion
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Seismology: Seismic Waves - Surface waves (Two Types: Love and Rayleigh Waves) + Travel along outer part of Earth
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Locating the Source of Earthquakes
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The Epicenter Is Located Using Three or More Seismographs
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Determining the Size of Earthquakes
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Seismic Intensity Map, Loma Prieta, 1989
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Measuring the Size of Earthquakes • Magnitude scales
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Earthquake Destruction
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Can Earthquakes Be Predicted?
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Seismic Gaps: Tools for Forecasting
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Paleoseismology: The Study of Prehistoric
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Review: Body Waves versus Surface Waves
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Paths that Seismic Waves Follow through Earth
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Earth's Layered Structure
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Meteorites
Description:
Explore the fascinating world of earthquakes and Earth's interior in this 51-minute geology lecture. Delve into the mechanics of faults, seismic wave propagation, and earthquake measurement techniques. Learn about different types of faults, seismographs, and how to locate earthquake epicenters. Examine the various scales used to measure earthquake magnitude and intensity, and discover the challenges of earthquake prediction. Investigate seismic gaps, paleoseismology, and the paths seismic waves follow through Earth's layered structure. Gain insights into plate tectonics, earthquake destruction, and the study of meteorites as they relate to understanding our planet's interior.