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23 Cards in this Set
- Front
- Back
Tectonic Earthquakes
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caused by the stresses put on the plates (colliding, pulled apart, etc.) most common
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Volcanic Earthquakes
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as magma moves from the ground the rocks around it vibrate most common
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Collapse Earthquakes
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caves, landslides -> large blocks of rock moving create seismic activity
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Explosion Earthquakes
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Nuclear detonations, fuel plant explosions
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Focus
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where the earthquake originates on the fault
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Wave Front
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where the seismic waves have yet to reach
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Epicenter
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the focus projected onto a surface map
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Ray Path
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vector of one of the directions the wave travelled
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Body Waves
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move through the interior of the earth
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Surface Waves
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move along the surface of the earth
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Body vs. Surface Waves
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of the three types of earthquake waves, two travel though the interior of the planet and one travels along the surface
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Shear Wave
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- particle move up/down or left/right (can be surface or body waves) (string)
- shear body wave - Rayleigh Wave = R-wave - Love Wave = L-wave |
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Shear Body Wave
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secondary wave (s-wave), second highest speed
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Compressional Wave
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- particle move back and forth parallel to the direction of wave motion (slinky), move faster than shear waves
- Compressional Body Wave |
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Body Waves
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- Shear Body Waves
- Compressional Body Waves |
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Surface Waves
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- expressed at the surface and dies down with depth, slowest of all earthquake waves, cause the most damage (ground moves up and down, side to side)
- Rayleigh Wave = R-wave - Love Wave = L-wave |
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Seismometer
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measures earthquakes, recording called a seismogram
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Mercalli Intensity Scale
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defines the intensity of an earthquake by the amount of damage it causes. Intensity ranges fro I to XII, somewhat subjective because number depends on damage, varies with distance. Measure of relative strength perceived and felt
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Richter Magnitude Scale
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- measures the relative amount of energy releases by determining the amplitude of the largest ground motion
- The limit of the Richter Scale is technically 0 to infinity but the scale become less and less precise past 8.9 - An increase of one unit of magnitude equals about 33 times more energy - So a magnitude 8 earthquake does not release twice as much energy as a magnitude 4 quake but 1 million times as much |
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Modern Moment Magnitude Scale
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- measures the total energy released by a quake more precisely than the historical richter scale
- Can precisely measure very large earthquakes including >8.9 - Calculation of energy in part includes: - Length of the fault rupture - Area of rupture surface |
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Hazards
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- Ground Shaking
- Landslides - Liquefaction - Fire - Disease |
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Liquefaction
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- ground vibration cause water-logged soils and clayey sediments to become a slurry of mud and water
- Sandblows (sand volcanoes): water rushes to the surface, water can be boiling |
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Disease
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disruption of infrastructure, lack of sanitation, food and water can quickly lead to outbreaks of disease
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