Earthquake Notes2.ppt....................
 Earthquake = the shaking and
trembling that results from
movement of rock beneath
Earth’s surface
 Focus = area beneath Earth’s
surface where rock under stress
breaks and causes an
earthquake
 Epicenter = point on the
surface directly above the focus
A. Earthquakes produce vibrations called
Waves.
B. Waves carry energy.
C. Seismic waves are vibrations that travel
through Earth carrying energy released
during an earthquake.
D. Seismic waves carry energy from an
earthquake away from the focus, through
Earth’s interior and across the surface.
E. Three main categories of Waves:
Primary Waves (P waves)
Secondary Waves (S waves)
Surface Waves
 The first waves to arrive are Primary waves.
› P waves compress and expand the ground.
 After P waves come Secondary waves.
› S waves are seismic waves that vibrate from Side to
Side as well as up and down.
 When P waves reach the surface, some of them
become Surface waves.
› Surface waves move more slowly than P or S waves
but they produce severe ground movements.
Earthquake Notes2.ppt....................
Earthquake Notes2.ppt....................
 There are at least 3 different measures
for rating earthquakes.
 Two methods for measurement:
› Mercalli Scale
› Richter Scale
 Mercalli Scale = Rate earthquakes on the
level of damage at a certain place
Earthquake Notes2.ppt....................
 Richter Scale = rating of an
earthquake’s magnitude
based on the size of the
earthquake’s seismic waves
› Magnitude is a number
geologists assign to an
earthquake based on the
earthquake’s size
› the seismic waves are
measured by a seismograph
 Comparing Magnitudes
› An earthquake’s magnitude tells Scientists
how much energy was released by the
earthquake
› Earthquakes with a Magnitude of 6 cause?
 Moderate damage
 32 times the energy of a
Magnitude 5 Quake
 Geologists use seismic waves to locate
an earthquake’s epicenter.
Recording
Station
Time Difference
in the arrival time
of P- wave and
S- wave
(seconds)
Distance of
epicenter from
the stations
Occidental
Mindoro
40
Samar 32
Zamboanga
del Norte
36
ACTIVITY TIME
 1. Is earthquake predictable? Explain
your answer.
 2. What is the minimum number of
seismic stations necessary to locate an
epicenter?
 3. How can you determine the epicenter
of an earthquake using data from
seismic stations worldwide?
(COPY AND ANSWER THIS AFTER COPYING
NUMBER 5 ON PAGE 9)
 4. Where was the epicenter of this
earthquake located?
 5. Your circle must not have
intersected precisely at one point.
Other than the error in your
measurement, what are the possible
reasons for this? (Be specific.)

More Related Content

PPT
Earthquake Notes2.pptEarthquake Notes2.ppt
PPT
There are at least 3 different measures for rating earthquakes. Two methods ...
PPT
Earthquake Notes and its Classification.ppt
PPT
Differentiate focus and epicenter using f
PPT
Differentiate focus and epicenter using f
PPT
Geological hazards earthquake unit v
PPTX
EARTHQUAKE environment notes for geology.pptx
PPT
Earthquake basics
Earthquake Notes2.pptEarthquake Notes2.ppt
There are at least 3 different measures for rating earthquakes. Two methods ...
Earthquake Notes and its Classification.ppt
Differentiate focus and epicenter using f
Differentiate focus and epicenter using f
Geological hazards earthquake unit v
EARTHQUAKE environment notes for geology.pptx
Earthquake basics

Similar to Earthquake Notes2.ppt.................... (20)

PPTX
Earthquake , Tsunami and Subduction zone
PPSX
Introduction to Earthquake by JAWAD AHMED
PDF
EARTH EARTHQUAKES
PPTX
Earth quakes
PPTX
Ch.5.less.4.what are earthquakes and how do they occur
PPTX
Ch.5.less.4.what are earthquakes and how do they occur
PDF
Earthquakeppt 160308191544
PPTX
earthquake
PPTX
Earthquake ppt
PPT
Earthquakes and Seismic Waves.ppt
PPT
Earthquake Science - What They Are, How They're Formed
PPT
Final earthquake ppt.ppt
PPTX
earthquakeppt-160308191544 (1) (1).pptx
PPTX
earthquakeppt-160308191544.pptx
PPTX
EarthQuakes
PPTX
Earthquake ppt.pptx [Repaired].pptx
PPTX
EARTHQUAKES AND FAULTS
PPT
Earthquakes-and-Faults-Lectur science 7 grade 7 e.ppt
PPT
Earthquakes
Earthquake , Tsunami and Subduction zone
Introduction to Earthquake by JAWAD AHMED
EARTH EARTHQUAKES
Earth quakes
Ch.5.less.4.what are earthquakes and how do they occur
Ch.5.less.4.what are earthquakes and how do they occur
Earthquakeppt 160308191544
earthquake
Earthquake ppt
Earthquakes and Seismic Waves.ppt
Earthquake Science - What They Are, How They're Formed
Final earthquake ppt.ppt
earthquakeppt-160308191544 (1) (1).pptx
earthquakeppt-160308191544.pptx
EarthQuakes
Earthquake ppt.pptx [Repaired].pptx
EARTHQUAKES AND FAULTS
Earthquakes-and-Faults-Lectur science 7 grade 7 e.ppt
Earthquakes
Ad

Recently uploaded (20)

PPTX
Computer Architecture Input Output Memory.pptx
PDF
OBE - B.A.(HON'S) IN INTERIOR ARCHITECTURE -Ar.MOHIUDDIN.pdf
PPTX
20th Century Theater, Methods, History.pptx
PDF
Hazard Identification & Risk Assessment .pdf
PPTX
CHAPTER IV. MAN AND BIOSPHERE AND ITS TOTALITY.pptx
PPTX
Virtual and Augmented Reality in Current Scenario
PPTX
TNA_Presentation-1-Final(SAVE)) (1).pptx
PDF
LDMMIA Reiki Yoga Finals Review Spring Summer
PDF
Weekly quiz Compilation Jan -July 25.pdf
PPTX
Onco Emergencies - Spinal cord compression Superior vena cava syndrome Febr...
PPTX
Unit 4 Computer Architecture Multicore Processor.pptx
PDF
CISA (Certified Information Systems Auditor) Domain-Wise Summary.pdf
PDF
What if we spent less time fighting change, and more time building what’s rig...
PDF
Vision Prelims GS PYQ Analysis 2011-2022 www.upscpdf.com.pdf
PDF
MBA _Common_ 2nd year Syllabus _2021-22_.pdf
PDF
احياء السادس العلمي - الفصل الثالث (التكاثر) منهج متميزين/كلية بغداد/موهوبين
PDF
Paper A Mock Exam 9_ Attempt review.pdf.
PDF
Τίμαιος είναι φιλοσοφικός διάλογος του Πλάτωνα
PDF
Complications of Minimal Access-Surgery.pdf
PDF
1.3 FINAL REVISED K-10 PE and Health CG 2023 Grades 4-10 (1).pdf
Computer Architecture Input Output Memory.pptx
OBE - B.A.(HON'S) IN INTERIOR ARCHITECTURE -Ar.MOHIUDDIN.pdf
20th Century Theater, Methods, History.pptx
Hazard Identification & Risk Assessment .pdf
CHAPTER IV. MAN AND BIOSPHERE AND ITS TOTALITY.pptx
Virtual and Augmented Reality in Current Scenario
TNA_Presentation-1-Final(SAVE)) (1).pptx
LDMMIA Reiki Yoga Finals Review Spring Summer
Weekly quiz Compilation Jan -July 25.pdf
Onco Emergencies - Spinal cord compression Superior vena cava syndrome Febr...
Unit 4 Computer Architecture Multicore Processor.pptx
CISA (Certified Information Systems Auditor) Domain-Wise Summary.pdf
What if we spent less time fighting change, and more time building what’s rig...
Vision Prelims GS PYQ Analysis 2011-2022 www.upscpdf.com.pdf
MBA _Common_ 2nd year Syllabus _2021-22_.pdf
احياء السادس العلمي - الفصل الثالث (التكاثر) منهج متميزين/كلية بغداد/موهوبين
Paper A Mock Exam 9_ Attempt review.pdf.
Τίμαιος είναι φιλοσοφικός διάλογος του Πλάτωνα
Complications of Minimal Access-Surgery.pdf
1.3 FINAL REVISED K-10 PE and Health CG 2023 Grades 4-10 (1).pdf
Ad

Earthquake Notes2.ppt....................

  • 2.  Earthquake = the shaking and trembling that results from movement of rock beneath Earth’s surface  Focus = area beneath Earth’s surface where rock under stress breaks and causes an earthquake  Epicenter = point on the surface directly above the focus
  • 3. A. Earthquakes produce vibrations called Waves. B. Waves carry energy. C. Seismic waves are vibrations that travel through Earth carrying energy released during an earthquake.
  • 4. D. Seismic waves carry energy from an earthquake away from the focus, through Earth’s interior and across the surface. E. Three main categories of Waves: Primary Waves (P waves) Secondary Waves (S waves) Surface Waves
  • 5.  The first waves to arrive are Primary waves. › P waves compress and expand the ground.  After P waves come Secondary waves. › S waves are seismic waves that vibrate from Side to Side as well as up and down.  When P waves reach the surface, some of them become Surface waves. › Surface waves move more slowly than P or S waves but they produce severe ground movements.
  • 8.  There are at least 3 different measures for rating earthquakes.  Two methods for measurement: › Mercalli Scale › Richter Scale  Mercalli Scale = Rate earthquakes on the level of damage at a certain place
  • 10.  Richter Scale = rating of an earthquake’s magnitude based on the size of the earthquake’s seismic waves › Magnitude is a number geologists assign to an earthquake based on the earthquake’s size › the seismic waves are measured by a seismograph
  • 11.  Comparing Magnitudes › An earthquake’s magnitude tells Scientists how much energy was released by the earthquake › Earthquakes with a Magnitude of 6 cause?  Moderate damage  32 times the energy of a Magnitude 5 Quake
  • 12.  Geologists use seismic waves to locate an earthquake’s epicenter.
  • 13. Recording Station Time Difference in the arrival time of P- wave and S- wave (seconds) Distance of epicenter from the stations Occidental Mindoro 40 Samar 32 Zamboanga del Norte 36
  • 15.  1. Is earthquake predictable? Explain your answer.  2. What is the minimum number of seismic stations necessary to locate an epicenter?  3. How can you determine the epicenter of an earthquake using data from seismic stations worldwide? (COPY AND ANSWER THIS AFTER COPYING NUMBER 5 ON PAGE 9)
  • 16.  4. Where was the epicenter of this earthquake located?  5. Your circle must not have intersected precisely at one point. Other than the error in your measurement, what are the possible reasons for this? (Be specific.)

Editor's Notes

  • #2: Intro to Earthquakes http://www.youtube.com/watch?v=JrBaiPN6AW8
  • #3: Earthquakes http://www.youtube.com/watch?v=YPhXXgjFwmg
  • #4: Brain Pop Waves
  • #6: Refer to Textbook ….page 56 Math Skills Answer Questions 1 – 4 X axis is Distance from Epicenter and Y axis is arrival time 2. 7.5 minutes 4 minutes 2000 = 3.5 minutes and 4000 = 4.5 minutes
  • #8: Brain Pop Earthquakes
  • #10: How does a seismograph work? http://www.youtube.com/watch?v=Gbd1FcuLJLQ