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Seismology: Seismographs
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Classroom Contents
Geology - Earthquakes and Earth's Interior
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- 1 Earthquakes and Earth's Interior
- 2 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
- 3 Slippage along Faults
- 4 Types of Faults There are three major types of
- 5 How do Faults cause Earthquakes?
- 6 Principle of the Seismograph
- 7 Seismology: Seismographs
- 8 Seismology: Body Wave Motion
- 9 Seismology: Seismic Waves - Surface waves (Two Types: Love and Rayleigh Waves) + Travel along outer part of Earth
- 10 Locating the Source of Earthquakes
- 11 The Epicenter Is Located Using Three or More Seismographs
- 12 Determining the Size of Earthquakes
- 13 Seismic Intensity Map, Loma Prieta, 1989
- 14 Measuring the Size of Earthquakes • Magnitude scales
- 15 Earthquake Destruction
- 16 Can Earthquakes Be Predicted?
- 17 Seismic Gaps: Tools for Forecasting
- 18 Paleoseismology: The Study of Prehistoric
- 19 Review: Body Waves versus Surface Waves
- 20 Paths that Seismic Waves Follow through Earth
- 21 Earth's Layered Structure
- 22 Meteorites
