Title: Earthquakes
1Earthquakes
Chapter 22.5
2Real- Time Earthquake Data
- http//earthquake.usgs.gov/
3EQs
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)
4Stress 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
5Low Temp. Pressure Near Crust
High Temps. Pressure
6Folds
Anticline up facing fold Syncline down ward
facing fold
7Faults
8Types 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
9Types of Faults
- 2. Strike slip
- Sliding Horizontal Movement
- 3. Oblique slipdip-slip strike slip combined
10Plate Boundary Convergent
Interpretation of Tectonic History
Divergent
Transform
Normal
Thrust/Reverse
Strike-Slip
11EQ 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.
12SEISMOGRAPHS
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
133 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.
14Seismic 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
15Seismic 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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17Seismic 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
18Rating Earthquakes
- Earthquakes are rated in terms of MAGNITUDE or
INTENSITY by different scales. - Moment Magnitude Scale
- Richter Scale
- Mercalli Scale
19Moment 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
20How much more energy does a 7.5 release compared
to a 4.5?
21Richter 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
22Measuring 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
23Mercali 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
24EFFECTS OF EQs
- Deaths Injuries but mostly from collapsing
structures - Damage to buildings structures (collapse)
- Underground water and gas pipes break floods
fires - Landslides
- Tsunamis
25Seismic 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
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27A
- 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.
29B
- 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)
30G
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.
3110. A. What type of fault can you see in this
picture ? B. Could this location be an
ancient subduction zone? Why or why not?
3211. A. What type of fault can you see in this
picture ? B. What type of plate boundary
produces these faults?
3312. 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?
3413. A. What type of fault can you see in this
picture ? B. What type of forces produced this
fault? (There are 2 forces)
35Latest Quakes
- http//earthquake.usgs.gov/eqcenter/recenteqsww/Qu
akes/quakes_all.php - Top Ten Lists
- http//earthquake.usgs.gov/eqcenter/top10.php
36Links
- 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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