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Earthquakes

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Title: Earthquakes


1
Earthquakes
Chapter 22.5
2
Real- Time Earthquake Data
  • http//earthquake.usgs.gov/

3
EQs
EQ Movement of Es lithosphere that occurs when
rocks in the lithosphere suddenly shift,
releasing stored energy. EQs occur b/c stress
forces of have exceeded the strength of
rock. Stress builds when rocks along 2 sides of a
fault snag and lock (friction) as stress
builds so does POTENTIAL ENERGY IN
ROCKS When rocks are strained beyond limit
they break move. (Potential ? Kinetic Energy in
form of seismic waves)
4
Stress Strain on Rocks
Stress Force that squeezes rocks together,
pulls them apart, pushes in diff.
directions. Stress causes strain or deformation
(change in shape or volume) of rock
5
Low Temp. Pressure Near Crust
High Temps. Pressure
6
Folds
Anticline up facing fold Syncline down ward
facing fold
7
Faults
8
Types of Faults
  • 1. Dip SlipMotion up or down fault surface
  • Reverse or Thrust Hanging wall moves UP.
  • b. Normal Hanging wall moves DOWN

http//www.windows.ucar.edu/tour/link/earth/geolo
gy/fault.html
9
Types of Faults
  • 2. Strike slip
  • Sliding Horizontal Movement
  • 3. Oblique slipdip-slip strike slip combined

10
Plate Boundary Convergent
Interpretation of Tectonic History
Divergent
Transform
Normal
Thrust/Reverse
Strike-Slip
11
EQ Vibrations
  • EQ vibrations begin at a point called a FOCUS.
  • Vibrations travel from focus through the earths
    crust as waves.
  • Surface directly above the focus is called the
    epicenter.
  • These waves can be detected and measured on
    earths surface with a SEISMOGRAPH.

12
SEISMOGRAPHS
Instrument that measures records EQ waves.
Strength of EQ waves is referred to as MAGNITUDE.
Wave Motion http//sunshine.chpc.utah.edu/labs/s
eismic/index.htm?ASPIRE_Session964f1ed30b7e49ceb8
1bd77f444d9230
13
3 Types of Seismic Waves
  • 1. Primary Waves (P waves)
  • 2. Secondary Waves (S waves)
  • Surface Waves
  • Each wave originates from the FOCUS of the
    earthquake.
  • Each wave travels in a different way, at
    different speeds, and causes different amounts of
    destruction.

14
Seismic Waves vibrations produced by energy
released during EQ
  • P Waves Primary Wave
  • Arrives 1st Travels FASTER
  • Longitudinal / Travel in direction of wave
    motion.
  • Compress Expand like accordion (like sound
    waves)
  • Move through Solids Liquids
  • Virtual EQs http//www.sciencecourseware.org/Virt
    ualEarthquake/VQuakeExecute.html
  • Seismic Waves http//www.geo.mtu.edu/UPSeis/wav
    es.html

15
Seismic Waves
  • S Waves Secondary
  • Transverse Material vibrates perpendicular (rt
    angles) to wave motion
  • What you FEEL in an EQ
  • Rock moves up down or side to side
  • Arrive after P
  • Move only through SOLIDS

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17
Seismic Waves Surface Waves
  • Surface Waves develop when vibrations reach
    surface
  • Slower than P waves
  • Most destructive Different types of motion
  • More P S wave animations http//www-rohan.sdsu
    .edu/rmellors/lab8/l8maineq.htm
  • Video clip http//news.bbc.co.uk/1/hi/sci/tech/4
    126809.stm

18
Rating Earthquakes
  • Earthquakes are rated in terms of MAGNITUDE or
    INTENSITY by different scales.
  • Moment Magnitude Scale
  • Richter Scale
  • Mercalli Scale

19
Moment Magnitude Scale
  • Uses a seismogram
  • Rates on scale from 1- 10
  • Looks at Eqs in terms of ENERGY
  • Each releases 31 times more ENERGY than the
    before it.
  • Example
  • A 6 releases 31 times more energy than a 5,
    and a 5 releases 31 times more energy than a 4.
    The energy difference between a 4 and a 6 EQ on
    the richter scale is 31 X 31 961

20
How much more energy does a 7.5 release compared
to a 4.5?
  • Show your work here.

21
Richter Scale
  • Uses a seismogram
  • Rates on scale from 1- 10
  • Looks at Eqs in terms of the SIZE OF THE WAVES
  • 1 3 Small earthquake waves very little
    shaking
  • 4 6 Moderate earthquakes noticeable shaking
    and some damage
  • 7 - 10 BIG Earthquakes Very destructive

22
Measuring EQs Mercali Intensity Scale
  • Measures observed effects of Earthquake on a 1
    12 scale
  • Degree of shaking and damage
  • Not an actual measure of seismic waves
  • Link
  • http//www.abag.ca.gov/bayarea/eqmaps/doc/mmi.html

23
Mercali Intensity Scale
  • Measures observed RESULTS of Earthquake on a 1
    12 scale
  • Degree of shaking and DAMAGE to structures
  • Dont need a seismogram
  • Link
  • http//www.abag.ca.gov/bayarea/eqmaps/doc/mmi.html

24
EFFECTS OF EQs
  • Deaths Injuries but mostly from collapsing
    structures
  • Damage to buildings structures (collapse)
  • Underground water and gas pipes break floods
    fires
  • Landslides
  • Tsunamis

25
Seismic Waves are used to Study Earths Interior
P and S waves are bent and their velocities are
affected as they move through material of varying
density
Link http//sunshine.chpc.utah.edu/labs/seismic/
index.htm?ASPIRE_Session964f1ed30b7e49ceb81bd77f4
44d9230
26
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27
A
  • What type of fold is shown here? (Anticline or
    Syncline)
  • 2. Would these folds be created in a DUCTILE
    (high temp. pressure, deeper in crust) or
    BRITTLE (low temp pressure, at surface)
    environment?

28
  • 3. These folds in Newfoundland New Jersey would
    have be produced
  • When Pangaea assembled 240 Ma.
  • When Pangaea broke apart 100 Ma
  • During the ice age as glacial ice sheets
    retreated 10 Ka
  • They are currently being produced by New Jerseys
    current tectonic activity.
  • 4. Support your answer to 2 with a reason.

29
B
  • Is this a dip-slip or strike slip fault? If
    dip-slip say what type of dip-slip (Thrust or
    Normal).
  • Is this fold produced by compressional
    extensional or shearing forces?
  • What type of plate boundary would you expect to
    find these faults? (Convergent Divergent
    Transform)

30
G
H
  • 8. Which fault would be produced by shearing
    forces?
  • 9. Would fault H be made in an ancient rift
    valley or a mountain building zone? Support your
    answer with a reason.

31
10. A. What type of fault can you see in this
picture ? B. Could this location be an
ancient subduction zone? Why or why not?
32
11. A. What type of fault can you see in this
picture ? B. What type of plate boundary
produces these faults?
33
12. A. What type of fault can you see in this
picture ? B. Could this location be an
ancient convergent plate boundary? Why or why
not?
34
13. A. What type of fault can you see in this
picture ? B. What type of forces produced this
fault? (There are 2 forces)
35
Latest Quakes
  • http//earthquake.usgs.gov/eqcenter/recenteqsww/Qu
    akes/quakes_all.php
  • Top Ten Lists
  • http//earthquake.usgs.gov/eqcenter/top10.php

36
Links
  • Virtual Earthquakes
  • http//www.sciencecourseware.org/VirtualEarthquake
    /VQuakeExecute.html
  • Wave Types http//www.geo.mtu.edu/UPSeis/waves.htm
    l
  • Triangulation Hearing EQs
  • http//www.seismo.unr.edu/ftp/pub/louie/class/100/
    seismic-waves.html
  • More virtual seismograms
  • http//www-rohan.sdsu.edu/rmellors/lab8/l8maineq.
    htm
  • Earthquakes outline subducting slab Interactive
    Web Lab
  • http//openlearn.open.ac.uk/mod/resource/view.php?
    id172185

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