SlideShare a Scribd company logo
1 of 19
FOCUS
CA- California K-12 Academic Content Standards
Subject : Science
Grade : Grades Nine Through Twelve
Area : Earth Sciences
Sub-Strand : Dynamic Earth Processes
Concept 3: Plate tectonics operating over geologic time has changed the patterns of land, sea, and
mountains on Earth’s surface. As the basis for understanding this concept:
a: Students know features of the ocean floor (magnetic patterns, age, and sea-floor topography) provide
evidence of plate tectonics.
b: Students know the principal structures that form at the three different kinds of plate boundaries.
c: Students know how to explain the properties of rocks based on the physical and chemical conditions in
which they formed, including plate tectonic processes.
d: Students know why and how earthquakes occur and the scales used to measure their intensity and
magnitude.
1. Compare and contrast plate boundaries:
   convergent, divergent, and transform
2. Learn about the causes and effects of
   earthquakes and where they occur
 Seismologist- scientist who studies seismic
 waves
 *Convection Currents move tectonic plates.
 *Convection Currents in the Earth are caused
 by the Earth’s hot inner core heating the
 magma within the mantle.
   The movement of tectonic plates is related to the distribution of
    heat by convection currents in the mantle.
   *A Fault is a fracture, or break, in Earth’s
    Lithosphere.

     Along parts of the fault, the rocks on either side may
      slide along slowly and constantly.

     Along other parts of the fault, the rocks may stick, or
      lock together.

     The rocks bend as stress is put on them.
 *Stress: Force exerted when an object
 presses on, pulls on, or pushes against
 another object.

  *As stress increases, the rocks break free. A
   sudden release of stress in the Lithosphere causes
   an earthquake
 *An Earthquake is the shaking of the ground
 caused by a sudden movement of large blocks
 of rock along a fault.

 *Most faults are located along tectonic plate
 boundaries, therefore, most earthquakes
 occur at those points.

   The rocks that move are much smaller than the
   tectonic plate.
 Tectonic Plates can be thousands of kilometers
   long.
  During even a powerful earthquake the rocks
   may only move a few meters past each other
   along a distance of several hundred kilometers.
 *The strength of an earthquake depends
 in part on:
  *How much stress builds up (potential energy)
   before the rocks move.
  *The distance the rocks move along the fault.
 80% of all earthquakes occur in a belt around
 the edges of the Pacific Ocean.

   In the U.S. the best-known Fault in this belt is the
   San Andreas Fault in CA.

   The Fault forms part of the boundary between the
   North American Plate and the Pacific Plate.
 The San Andreas, unlike many other Faults, can be
    seen on the surface of the ground.
   Earthquakes also occur along Faults within plates.
   All Earthquakes occur in the Lithosphere where the
    rocks are cold, hard and brittle.
   Below the Lithosphere is the hot malleable, and in
    spots, molten.
   A few Earthquakes occur far below the normal depth
    of the Lithosphere because the plates being
    Subducted are still cold and rigid enough to break.
AQ

        All Earthquakes occur in the Lithosphere where the rocks
         are cold, hard and brittle
 A      Below the Lithosphere is the hot malleable, and in spots,
         molten.
Can you identify which of the plates are only made of oceanic crust?
   Use usgs.gov to find earthquakes in real-time to map
    the tectonic plates.
 Write three questions from this section, look
 in the book or on the Internet for the
 answers.
   Pg 543-551

More Related Content

What's hot

Earth Science 4.2 : Restless Continents
Earth Science 4.2 : Restless ContinentsEarth Science 4.2 : Restless Continents
Earth Science 4.2 : Restless ContinentsChris Foltz
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonicsmartalpz
 
Plate tectonics, earthquakes, and volcanism final(3)1
Plate tectonics, earthquakes, and volcanism final(3)1Plate tectonics, earthquakes, and volcanism final(3)1
Plate tectonics, earthquakes, and volcanism final(3)1Grace Espago
 
Tectonics: Plate Tectonic Theory history
Tectonics: Plate Tectonic Theory historyTectonics: Plate Tectonic Theory history
Tectonics: Plate Tectonic Theory historygeomillie
 
2.4 tectonic plate boundaries
2.4 tectonic plate boundaries 2.4 tectonic plate boundaries
2.4 tectonic plate boundaries mojavehack
 
Earth Science 4.3 : The Theory of Plate Tectonics
Earth Science 4.3 : The Theory of Plate TectonicsEarth Science 4.3 : The Theory of Plate Tectonics
Earth Science 4.3 : The Theory of Plate TectonicsChris Foltz
 
Concept of isostatic adjustment and isostatic models
Concept of isostatic adjustment and isostatic models Concept of isostatic adjustment and isostatic models
Concept of isostatic adjustment and isostatic models parag sonwane
 
Platetectonics theory
Platetectonics theoryPlatetectonics theory
Platetectonics theoryanayamalik18
 
Ii. d. deformation of the crust
Ii. d. deformation of the crustIi. d. deformation of the crust
Ii. d. deformation of the crustMarian Santos
 
Convection in the mantle
Convection in the mantle Convection in the mantle
Convection in the mantle 0000976589
 
Crustal Movement
Crustal MovementCrustal Movement
Crustal MovementnoraMs
 
Study of plate tectonics of the earth, or plate movement,
Study of plate tectonics of the earth, or plate movement, Study of plate tectonics of the earth, or plate movement,
Study of plate tectonics of the earth, or plate movement, Jahangir Alam
 
Plate tectonics theory
Plate tectonics theoryPlate tectonics theory
Plate tectonics theorycesarbuot
 
Plate Tectonics: History and Boundaries
Plate Tectonics: History and BoundariesPlate Tectonics: History and Boundaries
Plate Tectonics: History and Boundariesgpc2717
 
Natural Disasters Topic 3 (Plate Tectonics)
Natural Disasters Topic 3 (Plate Tectonics)Natural Disasters Topic 3 (Plate Tectonics)
Natural Disasters Topic 3 (Plate Tectonics)William W. Little
 

What's hot (20)

Earth Science 4.2 : Restless Continents
Earth Science 4.2 : Restless ContinentsEarth Science 4.2 : Restless Continents
Earth Science 4.2 : Restless Continents
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
Plate tectonics, earthquakes, and volcanism final(3)1
Plate tectonics, earthquakes, and volcanism final(3)1Plate tectonics, earthquakes, and volcanism final(3)1
Plate tectonics, earthquakes, and volcanism final(3)1
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
Tectonics: Plate Tectonic Theory history
Tectonics: Plate Tectonic Theory historyTectonics: Plate Tectonic Theory history
Tectonics: Plate Tectonic Theory history
 
2.4 tectonic plate boundaries
2.4 tectonic plate boundaries 2.4 tectonic plate boundaries
2.4 tectonic plate boundaries
 
Earth Science 4.3 : The Theory of Plate Tectonics
Earth Science 4.3 : The Theory of Plate TectonicsEarth Science 4.3 : The Theory of Plate Tectonics
Earth Science 4.3 : The Theory of Plate Tectonics
 
Concept of isostatic adjustment and isostatic models
Concept of isostatic adjustment and isostatic models Concept of isostatic adjustment and isostatic models
Concept of isostatic adjustment and isostatic models
 
Platetectonics theory
Platetectonics theoryPlatetectonics theory
Platetectonics theory
 
Ii. d. deformation of the crust
Ii. d. deformation of the crustIi. d. deformation of the crust
Ii. d. deformation of the crust
 
Convection in the mantle
Convection in the mantle Convection in the mantle
Convection in the mantle
 
Geodynamics
GeodynamicsGeodynamics
Geodynamics
 
Crustal Movement
Crustal MovementCrustal Movement
Crustal Movement
 
Study of plate tectonics of the earth, or plate movement,
Study of plate tectonics of the earth, or plate movement, Study of plate tectonics of the earth, or plate movement,
Study of plate tectonics of the earth, or plate movement,
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
Plate tectonics theory
Plate tectonics theoryPlate tectonics theory
Plate tectonics theory
 
Plate Tectonics: History and Boundaries
Plate Tectonics: History and BoundariesPlate Tectonics: History and Boundaries
Plate Tectonics: History and Boundaries
 
Diastrophism
DiastrophismDiastrophism
Diastrophism
 
Natural Disasters Topic 3 (Plate Tectonics)
Natural Disasters Topic 3 (Plate Tectonics)Natural Disasters Topic 3 (Plate Tectonics)
Natural Disasters Topic 3 (Plate Tectonics)
 

Similar to Earthquakes

Sec.2 slow motion on planet earth
Sec.2 slow motion on planet earthSec.2 slow motion on planet earth
Sec.2 slow motion on planet earthHamdy Karim
 
Quakes by Matthew Falzon, 3.05
Quakes by Matthew Falzon, 3.05Quakes by Matthew Falzon, 3.05
Quakes by Matthew Falzon, 3.05geographystudents
 
2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backupharvey09
 
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate Boundary
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate BoundaryWHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate Boundary
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate BoundaryUday Kumar Shil
 
Forces within earth
Forces within earthForces within earth
Forces within earthsaugusto
 
Grade 10_science1stquartermodule1.pptx
Grade 10_science1stquartermodule1.pptxGrade 10_science1stquartermodule1.pptx
Grade 10_science1stquartermodule1.pptxErlenaMirador1
 
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)DARYL (MONKAYO NHS)
 
g10science1stquartermodule1-200502160553 (2).pdf
g10science1stquartermodule1-200502160553 (2).pdfg10science1stquartermodule1-200502160553 (2).pdf
g10science1stquartermodule1-200502160553 (2).pdfKhaoriVladir
 

Similar to Earthquakes (20)

Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
Sec.2 slow motion on planet earth
Sec.2 slow motion on planet earthSec.2 slow motion on planet earth
Sec.2 slow motion on planet earth
 
Plate Tectonics.ppt
Plate Tectonics.pptPlate Tectonics.ppt
Plate Tectonics.ppt
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
Quakes by Matthew Falzon, 3.05
Quakes by Matthew Falzon, 3.05Quakes by Matthew Falzon, 3.05
Quakes by Matthew Falzon, 3.05
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
unit iii ppt.pptx
unit iii ppt.pptxunit iii ppt.pptx
unit iii ppt.pptx
 
2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup
 
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate Boundary
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate BoundaryWHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate Boundary
WHAT IS A PLATE? MAJOR PLATES. Types of Earth’s Crust. Plate Boundary
 
Forces within earth
Forces within earthForces within earth
Forces within earth
 
Grade 10_science1stquartermodule1.pptx
Grade 10_science1stquartermodule1.pptxGrade 10_science1stquartermodule1.pptx
Grade 10_science1stquartermodule1.pptx
 
Earthquake plates
Earthquake  platesEarthquake  plates
Earthquake plates
 
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)
PLATE TECTONICS(GRADE10SCIENCE 1STQUARTER MODULE1)
 
g10science1stquartermodule1-200502160553 (2).pdf
g10science1stquartermodule1-200502160553 (2).pdfg10science1stquartermodule1-200502160553 (2).pdf
g10science1stquartermodule1-200502160553 (2).pdf
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
CSEC GEOGRAPHY
CSEC GEOGRAPHY CSEC GEOGRAPHY
CSEC GEOGRAPHY
 
Diastrophism
DiastrophismDiastrophism
Diastrophism
 
Webquest answers
Webquest answersWebquest answers
Webquest answers
 
Plate Tectonics Theory.pdf
Plate Tectonics Theory.pdfPlate Tectonics Theory.pdf
Plate Tectonics Theory.pdf
 
plate tectonic 2.pptx
plate tectonic 2.pptxplate tectonic 2.pptx
plate tectonic 2.pptx
 

More from Emily Neistadt

Introduction to Theory of Evolution
Introduction to Theory of EvolutionIntroduction to Theory of Evolution
Introduction to Theory of EvolutionEmily Neistadt
 
Exploring dominant and recessive traits
Exploring dominant and recessive traitsExploring dominant and recessive traits
Exploring dominant and recessive traitsEmily Neistadt
 
Exploring dominant and recessive traits
Exploring dominant and recessive traitsExploring dominant and recessive traits
Exploring dominant and recessive traitsEmily Neistadt
 
Create an earth’s layers poster
Create an earth’s layers posterCreate an earth’s layers poster
Create an earth’s layers posterEmily Neistadt
 
Comparing Atoms and Periodic Table
Comparing Atoms and Periodic TableComparing Atoms and Periodic Table
Comparing Atoms and Periodic TableEmily Neistadt
 
Structure of the nervous system
Structure of the nervous systemStructure of the nervous system
Structure of the nervous systemEmily Neistadt
 
Creating a Science Fair Project
Creating a Science Fair ProjectCreating a Science Fair Project
Creating a Science Fair ProjectEmily Neistadt
 
Properties of Liquids and Gasese
Properties of Liquids and GaseseProperties of Liquids and Gasese
Properties of Liquids and GaseseEmily Neistadt
 
Classification of Matter
Classification of MatterClassification of Matter
Classification of MatterEmily Neistadt
 

More from Emily Neistadt (20)

Conservation
ConservationConservation
Conservation
 
Biodiversity
Biodiversity Biodiversity
Biodiversity
 
Introduction to Theory of Evolution
Introduction to Theory of EvolutionIntroduction to Theory of Evolution
Introduction to Theory of Evolution
 
Surface of the Earth
Surface of the EarthSurface of the Earth
Surface of the Earth
 
Types of Volcanoes
Types of VolcanoesTypes of Volcanoes
Types of Volcanoes
 
Volcanoes chapter 29
Volcanoes chapter 29Volcanoes chapter 29
Volcanoes chapter 29
 
Exploring dominant and recessive traits
Exploring dominant and recessive traitsExploring dominant and recessive traits
Exploring dominant and recessive traits
 
Patterns of Heredity
Patterns of HeredityPatterns of Heredity
Patterns of Heredity
 
Genetics ii
Genetics iiGenetics ii
Genetics ii
 
Exploring dominant and recessive traits
Exploring dominant and recessive traitsExploring dominant and recessive traits
Exploring dominant and recessive traits
 
Create an earth’s layers poster
Create an earth’s layers posterCreate an earth’s layers poster
Create an earth’s layers poster
 
Atoms family
Atoms familyAtoms family
Atoms family
 
Comparing Atoms and Periodic Table
Comparing Atoms and Periodic TableComparing Atoms and Periodic Table
Comparing Atoms and Periodic Table
 
nervous system
nervous systemnervous system
nervous system
 
Structure of the nervous system
Structure of the nervous systemStructure of the nervous system
Structure of the nervous system
 
Atomic structure18.1
Atomic structure18.1Atomic structure18.1
Atomic structure18.1
 
Creating a Science Fair Project
Creating a Science Fair ProjectCreating a Science Fair Project
Creating a Science Fair Project
 
The muscular system
The muscular systemThe muscular system
The muscular system
 
Properties of Liquids and Gasese
Properties of Liquids and GaseseProperties of Liquids and Gasese
Properties of Liquids and Gasese
 
Classification of Matter
Classification of MatterClassification of Matter
Classification of Matter
 

Earthquakes

  • 2. CA- California K-12 Academic Content Standards Subject : Science Grade : Grades Nine Through Twelve Area : Earth Sciences Sub-Strand : Dynamic Earth Processes Concept 3: Plate tectonics operating over geologic time has changed the patterns of land, sea, and mountains on Earth’s surface. As the basis for understanding this concept: a: Students know features of the ocean floor (magnetic patterns, age, and sea-floor topography) provide evidence of plate tectonics. b: Students know the principal structures that form at the three different kinds of plate boundaries. c: Students know how to explain the properties of rocks based on the physical and chemical conditions in which they formed, including plate tectonic processes. d: Students know why and how earthquakes occur and the scales used to measure their intensity and magnitude.
  • 3. 1. Compare and contrast plate boundaries: convergent, divergent, and transform 2. Learn about the causes and effects of earthquakes and where they occur
  • 4.  Seismologist- scientist who studies seismic waves
  • 5.  *Convection Currents move tectonic plates.  *Convection Currents in the Earth are caused by the Earth’s hot inner core heating the magma within the mantle.
  • 6. The movement of tectonic plates is related to the distribution of heat by convection currents in the mantle.
  • 7. *A Fault is a fracture, or break, in Earth’s Lithosphere.  Along parts of the fault, the rocks on either side may slide along slowly and constantly.  Along other parts of the fault, the rocks may stick, or lock together.  The rocks bend as stress is put on them.
  • 8.  *Stress: Force exerted when an object presses on, pulls on, or pushes against another object.  *As stress increases, the rocks break free. A sudden release of stress in the Lithosphere causes an earthquake
  • 9.  *An Earthquake is the shaking of the ground caused by a sudden movement of large blocks of rock along a fault.  *Most faults are located along tectonic plate boundaries, therefore, most earthquakes occur at those points.  The rocks that move are much smaller than the tectonic plate.
  • 10.
  • 11.  Tectonic Plates can be thousands of kilometers long.  During even a powerful earthquake the rocks may only move a few meters past each other along a distance of several hundred kilometers.  *The strength of an earthquake depends in part on:  *How much stress builds up (potential energy) before the rocks move.  *The distance the rocks move along the fault.
  • 12.  80% of all earthquakes occur in a belt around the edges of the Pacific Ocean.  In the U.S. the best-known Fault in this belt is the San Andreas Fault in CA.  The Fault forms part of the boundary between the North American Plate and the Pacific Plate.
  • 13.
  • 14.  The San Andreas, unlike many other Faults, can be seen on the surface of the ground.  Earthquakes also occur along Faults within plates.  All Earthquakes occur in the Lithosphere where the rocks are cold, hard and brittle.  Below the Lithosphere is the hot malleable, and in spots, molten.  A few Earthquakes occur far below the normal depth of the Lithosphere because the plates being Subducted are still cold and rigid enough to break.
  • 15.
  • 16. AQ  All Earthquakes occur in the Lithosphere where the rocks are cold, hard and brittle A Below the Lithosphere is the hot malleable, and in spots, molten.
  • 17. Can you identify which of the plates are only made of oceanic crust?
  • 18. Use usgs.gov to find earthquakes in real-time to map the tectonic plates.
  • 19.  Write three questions from this section, look in the book or on the Internet for the answers.  Pg 543-551