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earthquake waves
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body waves
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p-waves
- speed 5 to 7 km/s
- formed by alternate expansion and contraction of bedrock
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s-waves
- slower than p-waves
- formed from sheer stress and move the materials they pass through in a vertical or horizontal
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surface waves
- travel at or near the ground
- cause rolling or sweeping motion
- velocity is slower than that of body waves
- despite slow speed,cause considerable damage to construction as it causes strong ground movement
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detecting earthquakes
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Chinese seismograph
- 2000 years ago Chinese studied earthquake waves and to determine the direction
- hollow jar,heavy weight in jar suspended,metal balls in each dragon,which when opened falls in the mouth of the frog
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modern seismograph
- uses heavy weight with a pen on rolls of paper
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plate boundaries
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spreading zones
- molten rock rises pushing two plates apart
- they are mostly found in oceans
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transform faults
- plates slide past each other
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subduction zones
- one plate overrides the other
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6000 earthquakes every year
- 500 felt
- 15 cause damage
- 10000 people die every year
- oldest record of an earthquake from Shang dynasty,Chinese 3000 years ago