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shaking of the ground caused, most often, by the sudden release of energy stored in elastically-strained rocks (Elastic Rebound Theory) |
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the place within the Earth where energy is released |
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the point on the Earth’s surface directly above the focus |
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vibrational energy waves that travel outward in all directions from the focus. |
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machine used to measure seismic waves |
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data produce by a seismograph |
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1. travel along earth's surface 2.slowest seismic wave at 2.5 km (1.5 miles) per second 3.responsible for much earthquake damage |
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seismic waves that travel through the interior of the Earth |
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1.compressional wave. 2.fastest seismic waves 6 km (4 miles) per second. 3.transmitted through solids and liquids |
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1.shear wave 2.slower at 3.5 km (2 miles) per second 3.transmitted only through solids |
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rocks move up and down perpendicular to the direction of the wave |
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alternating compression and expansion of the rock in the direction of the wave |
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Locating an earthquake's epicenter |
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1.Distance of a seismograph from the epicenter is determined by the difference in arrival times of P and S waves. 2.Data from 3 seismic stations is used to triangulate the location of the epicenter |
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1.Mercalli Scale 2.Richter Scale 3.Moment Magnitude Scale |
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based on damage to buildings |
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1.Based on amplitudes (wave heights) of the largest seismic waves 2.Logarithmic Scale |
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an increase of 1 on the scale: =10 fold increase in intensity and a =30 fold increase in energy released |
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a measure of earthquake strength base on: 1.rupture size 2.rock properties 3.amount of ground displacement along the fault |
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1.Most earthquakes occur along plate boundaries. 2.Depth of earthquake foci is related to type of plate boundary 3.Intraplate earthquakes |
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shallow (< 50 km). Mechanism is not well understood |
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1.Oceanic divergent boundaries 2.Continental rifts, collision zones and transforms 3.Subduction zones |
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1.deep (up to 700 km). 2.Wadati-Benioff zones |
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earthquakes that occur in the subducting slab |
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Continental rifts, collision zones and transforms |
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shallow to moderate (< 80 km) |
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Oceanic divergent boundaries |
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1.Ground Motion 2.Liquifaction 3.Landslides 4.Fire 5.Seismic Sea Waves (Tsunamis) |
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destruction varies: 1.Type of ground surface–soft sediments amplify vibrations more than solid rock 2.Structural design of buildings |
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1. Short-term Predictions 2. Long-term Predictions |
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1.Monitoring of phenomena such as: ground uplift and subsidence, strain in rocks 2.no reliable method |
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1.attempts to establish a recurrence interval 2.Seismic gaps |
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areas known to be under strain that have not produced earthquakes |
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based on: a.historically dated events b.dating of fault and quake activity |
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