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What is an Earthquake
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Over 30,000 happen each year worldwide that are strong enough to be felt Only about 75 major earthquakes take place each year many in remote regions Powerful Earthquake Reported in Costa Rica - YouTube
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A vibration of the Earth produced by the rapid release of energy Caused by slippage along a break in Earth’s crust
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Focus – point within earth where the earthquake starts › Waves are produced here Epicenter – location on the surface of Earth directly above the focus
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Faults – fractures in earth’s crust and mantle where movement has occurred
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Elastic rebound hypothesis – explanation for the release of energy stored in deformed rocks Earthquakes - Shock Waves Explained - YouTube
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Rocks are in the original position Stress builds up due to tectonic forces › Builds energy Energy is released › Earthquake Land rebounds into new position How Earthquakes Work - YouTube
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Aftershocks – movements that follow a major earthquake › Sometimes destroy structures weakened by the quake
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foreshocks - Small earthquakes happening before the major quake › Can be felt days or even years before
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Measuring Earthquakes
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Instruments that record earthquake waves
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2 types › Surface waves › Body waves seismic waves - YouTube
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Travel along earths outer layer Up and down as well as side to side motion Especially damaging to buildings Slower than body waves
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Pass through earth’s interior P waves – push – pull or compression waves › Faster than S waves S waves – shake particles at right angles › Cannot pass through gases or liquids S and P waves - YouTube
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Seismographs can be used to see the difference in velocity between p and s waves Interval between 1 st p wave arrival and 1 st s wave arrival › Longer the interval the further the distance from the earthquake Uses 3 or more seismographs
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2 types of measurement › Intensity Amount of shaking based on damage qualitative › Magnitude Calculations of energy released using seismographs Quantitative
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Based on amplitude of largest seismic wave Logarithmic › 10 fold increase in wave amplitude of 1 on the magnitude scale 5.0 is 10X greater than 4.0 Familiar but outdated
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Based on amount of displacement at a fault zone More precise Many different factors › Av. amount of movement › Area of surface break › Strength of broken rock Most widely used because it measures amount of energy released
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Destruction from earthquakes
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Depends on several factors › Intensity and duration › Nature of the material on which the structure is built › Design of the structure
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Where loosely consolidated sediments are saturated with water, stable soil can turn to a liquid during earthquakes Buildings may settle and collapse Underground storage tanks and sewage lines may float to the surface liquefaction
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Destructive waves › Aka tidal waves Not actually anything to do with tides Slab of ocean floor is displaced vertically along a fault Or when a quake sets off an underwater landslide Japan Tsunami first wave ground footage - YouTube
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Landslides – do the greatest damage › Soil and / or rock slopes fail Fire – gas and electrical lines may be cut › when water lines are also cut, fires cannot be stopped – San Francisco 1906
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