lecture outlines physical geology, 15/esubduction.rocks/storage for lecture notes/300 spr...
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Lecture Outlines
Physical Geology, 15/e
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Plummer, Carlson & Hammersley
Earthquakes
Physical Geology 15/e, Chapter 16
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Earthquake – a trembling or shaking of the ground caused by thesudden release of energy stored in the rocks beneath Earth’s surface
• energy is released in the form of seismic waves
• released from a position along a break between two rock masses (fault)
Elastic rebound theory - earthquakes are a sudden release of strainprogressively stored in rocks that bend until they finally break and movealong a fault
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Causes of Earthquakes
Focus – (or hypocenter) the point of initialbreakage and movement along a fault, whereseismic waves originate
Epicenter - point on Earth’s surfacedirectly above the focus
Two types of seismic waves:• body waves - travel outward from the
focus in all directions through Earth’sinterior
• surface waves - travel along Earth’ssurface away from the epicenter
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Seismic Waves
Body Waves• P wave - compressional (longitudinal) body wave
in which rock vibrates back and forth parallel tothe direction of wave propagation
• fast (4 to 7 km/sec) wave that is the first orprimary wave to arrive at recording station
• pass through solids and fluids
• S wave - shearing (transverse) body wave inwhich rock vibrates back and forth perpendicularto the direction of wave propagation
• slower (2 to 5 km/sec) wave that is the secondarywave to arrive at recording station
• pass through solids only
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Seismic Waves
Surface Waves
• Slowest type of seismicwaves produced byearthquakes
• Love waves – side-to-
side motion of the groundsurface, can’t travelthrough fluids
• Rayleigh waves –
ground moves in anelliptical path opposite thedirection of wave motion;extremely destructive tobuildings
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Seismic Waves
Seismometers – used to measure seismic waves
Seismographs – recording devices used to produce a permanent
record of the motion detected by seismometers
Seismograms – permanent paper (or digital) records of the
earthquake vibrations
• used to measure the earthquake strengths
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Locating and Measuring Earthquakes
Determining the Location ofan Earthquake
• Travel-time curve – used todetermine distance to focus
• based on time between first P- andS-wave arrivals
• P- and S-waves leave earthquakefocus at the same time
• P-wave gets farther and fartherahead of the S-wave with distanceand time from the earthquake
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Locating and Measuring Earthquakes
Determining the Location ofan Earthquake
• Plotting distances from 3 stationson a map, as circles with radiiequaling the distance from thequake, locates earthquakeepicenter
• Depth of focus beneath Earth’ssurface can also be determined
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Locating and Measuring Earthquakes
Measuring the “Size” of an Earthquake
Intensity – a measure of the effects an earthquake
produces (on both structures and people)
• Modified Mercalli Scale
• Range of I-XII
• Drawbacks
• Damage lessens with distance fromepicenter
• Damage also depends on severalother factors (type of geology,construction etc…)
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Locating and Measuring Earthquakes
Measuring the “Size” of Earthquakes
Magnitude – a measure of the amount of energyreleased by an earthquake by measuring theamplitude of seismic waves on a seismogram
•Richter scale
• Numerical scale of magnitudes
• Originally developed for shallowearthquakes in California
•Moment Magnitude Scale – moreobjective measure of energy released bya major earthquake
• uses rock strength, surface area of faultrupture, and amount of movement
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Locating and Measuring Earthquakes
Location and Size ofEarthquakes in the United States
• Most common in the western statesand Alaska
• Largest seismic risks or hazardsexist near the plate boundary alongthe Pacific coast and New Madrid,MO
• Seismic risk is determined based onthe assumption that large futureearthquakes will occur where theyhave occurred in the past
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Locating and Measuring Earthquakes
Ground motion – trembling and shakingof the land during an earthquake
Fire – from broken gas and water mains andfallen electrical wires
Ground Failure• Landslides – triggered by ground
shaking
• Liquefaction – occurs when water-saturated soil or sediment sloshes like aliquid during a quake
• Permanent displacement of theland surface – leaving fractures andscarps
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Earthquake-Related Hazards
Aftershocks•Small earthquakes that follow the main earthquake•Can cause considerable damage to alreadydamaged buildingsTsunamiSeismic sea waves caused by sudden upward ordownward movement of the sea floor duringsubmarine earthquakes
• generally produced by magnitude 8+ earthquakes• may also be generated by large undersea landslides
or volcanic explosions• travel across open ocean at speeds of >700 km/hr.• reach great heights in coastal areas with gently sloping
seafloor and funnel-shaped bays
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Earthquake-Related Hazards
Most earthquakes occur in narrow geographic belts which marktectonic plate boundaries
• important concentrations occur in the circum-Pacific andMediterranean-Himalayan belts
• shallow-focus earthquakes common along the crests of mid-oceanicridges
• nearly all intermediate- and deep-focus earthquakes occur in Benioffzones
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World Distribution of Earthquakes
• Rock motion is determined by studying seismograms from manylocations
• Each seismogram can identify whether the first motion was a push(up deflection) or pull (down deflection) at that location
• There are two possible solutions for any pattern of first motionsthat can be solved by knowing the fault orientation
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First-Motion Studies of Earthquakes
Earthquakes and Plate Boundaries• Plate boundaries are identified and defined by earthquakes
• Earthquakes occur at each of the three types of plate boundaries: divergent,transform, and convergent
Subduction Angle
• Determined by the horizontal and vertical distribution of earthquakes
• Controlled by plate density
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Earthquakes and Plate Tectonics
Earthquake Precursors and Prediction
• Microseisms – small tremors caused by small breaks in therocks
• Rock properties changes - such as magnetism, electricalresistivity, seismic velocity, and porosity
• Water level in wells
• Radon emission increases
• Animal behavior
• Foreshocks
• These all appear to be very inconsistent, making short termprediction difficult
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Earthquake Prediction and Forecasting
Earthquake Forecasting
•Paleoseismology – studies that determine where andwhen earthquakes have occurred and their size
•Study geologic record
•Digging trenches across fault zone
•Recurrence interval
•Seismic gaps – inactive segments along fault zone
•Slip rate along fault zones
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Earthquake Prediction and Forecasting
Reducing Earthquake Damageand Risk
• Monitoring the amount ofshaking and relaying shake mapinformation rapidly to guideemergency personnel to themost damaged areas
• Develop early warning systems
• Shut down gas lines, subways,trains etc…
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Earthquake Prediction and Forecasting
End of Chapter 16
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