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Earthquakes

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Meteors and Asteroids bombarded the Earth. Gravitational ... Instruments around the world record EQ. Records Earth movement by stationary mass on rotating drum ... – PowerPoint PPT presentation

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Title: Earthquakes


1
Earthquakes
  • And Earths Structure

2
Earths Structure
3
Origin of the Earth
  • Meteors and Asteroids bombarded the Earth
  • Gravitational compression
  • Density Stratified planet

4
Earths Interior
  • Core
  • dense
  • Iron and Nickel
  • Inner Core - solid
  • Outer Core - liquid
  • Mantle
  • Less dense than core
  • Iron and Magnesium silicates
  • Mostly solid
  • Upper mantle is partially molten
  • Crust
  • Outermost layer
  • Very thin and rigid
  • Continental granite
  • Density 2.8 g/cm3
  • Oceanic basalt
  • Density 3.0 g/cm3

5
Evidence of Internal Structure
  • Density
  • calculate density of Earth
  • Speculate on probable compositions
  • Meteorites
  • Use composition and age to determine composition
    and age of Earth
  • Seismic waves
  • Travel times and direction give indication of
    internal structure of Earth

6
Types of Seismic Waves
  • P waves
  • Primary waves
  • Push and pull movement
  • Travel fastest ( 6 km/sec)
  • Travel thru solids and liquids
  • S waves
  • Secondary waves
  • Move side-to-side
  • Slower ( 4 km/sec)
  • Travel thru solids only

7
Seismic Waves Through Earth
8
Parts of an Earthquake
  • Focus
  • place within earth where EQ originate
  • Epicenter
  • Location on surface directly above focus
  • Energy radiates in all directions from the focus
  • Energy is in the form of waves seismic waves

9
Seismic WavesLocating the Epicenter
  • Seismograph
  • Instruments around the world record EQ
  • Records Earth movement by stationary mass on
    rotating drum
  • Seismogram
  • Locate an epicenter
  • Determine magnitude

10
Seismogram
  • Help determine the epicenter
  • Measure the distance between P- and S-waves
  • This is the time difference in arrival times

11
Locating the Epicenter
  • Plot the time difference on y-axis (time interval)
  • Trace plot to blue line to determine distance to
    epicenter

12
Locating an Epicenter Triangulation
  • Measure that distance around the seismic station
  • The epicenter may be located anywhere on that line
  • A minimum of 3 seismic stations are needed to
    determine the epicenter

13
Earthquake StrengthRichter Scale
  • A measure of the strength of an earthquake or the
    amount of energy released

14
Determining Magnitude
  • Measure amplitude of the strongest wave
  • Amplitude is the height on paper
  • Plot distance between p- and s-wave
  • Plot amplitude
  • Connect plots to determine magnitude

15
Earthquake IntensityModified Mercalli Scale
  • Effects of an EQ vary from place to place
  • There is only 1 magnitude, but intensity can vary
  • Subjective scale

16
Intensity Map Loma Prieta 1989
17
Oakland, 1989
  • Oakland is farther from epicenter, but scored a 9
    on Intensity Scale

18
You are now a Seismologist!!
  • Virtual Earthquake Introduction
  • http//vcourseware5.calstatela.edu/VirtualEarthqua
    ke/VQuakeExecute/htm
  • Virtual Earthquake
  • http//sciencecourseware.org
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