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Earthquakes
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Warm-up What other damaging effects can be caused by earthquakes other than the earthquake itself?
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Earthquakes Mostly caused by plate tectonics
Two plates moving in different directions (usually transverse) Rock has a lot of friction, so they don’t slide easily Stress builds over time (energy storage) Stress is the force acting on a rock over a certain area When stress overcomes the strength of the rock, movement occurs The vibrations from this are felt as an earthquake (energy release)
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Stress Three kinds: Compression Tension Shear
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Faults Fracture in the crust along which the earth moves 3 kinds
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Reverse fault
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Normal Fault
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Strike-Slip Fault
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Anatomy of an earthquake
Focus: Where the actual earthquake occurred Epicenter: The point on the surface directly above the focus
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Seismic waves 3 types, all move differently Body waves: Surface waves
Primary Secondary Surface waves
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Primary waves P-waves Push-pull of rock First to arrive
Pass through the interior of the Earth Can pass through solid rock and liquids (water and molten rock) Body waves
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Secondary Waves S-waves Second to arrive
Pass through the interior of the Earth Only can pass through solids Body waves
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Surface Waves Last to arrive to arrive Travel through the surface only
Cause the most damage
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Seismometer Instruments that measure motion of the ground
Hanging mass (pendulum) stays still while the Earth moves under it The paper moves and the mass drags a marker across the paper The bigger the squiggle, the more energy released Records a seismogram, the graph showing the movement
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Seismogram
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Measuring Damage 3 scales: The Richter magnitude scale
The Modified Mercalli Intensity Scale The moment magnitude scale
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The Richter magnitude scale
assigns a magnitude number to quantify the size of an earthquake measured with a seismometer Measures how powerful it was Logarithmic scale (meaning each # is 10x worse so a 3 is 10x stronger than a 2 and 100x stronger than a 1)
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The Modified Mercalli Intensity Scale
The effect of an earthquake on the Earth's surface is called the intensity refers to the effects actually experienced at that place (damage assessment) Non-scientific, but relevant Very inaccurate judgement of the earthquake itself
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The moment magnitude scale
Most precise Measures actual energy released Based on the area of the fault that moved at the same moment as an earthquake
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