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EARTH SCIENCE REVIEW
DIFFERENCE BETWEEN
CONSTRUCTIVE AND DESTRUCTIVE
FORCES
 Constructive forces build up the earth’s surface
 Destructive wear away earth’s surface
LAYERS OF EARTH
   Lithosphere- consists of crust and top of mantle
     Separates into plates
     Meets at plate boundaries
   Asthenosphere- located under lithosphere; what
    the lithosphere glides on top of
PANGEA
 All the continents were once joined together in a
  super continent
 Continents fit together like puzzle pieces
SEA FLOOR SPREADING
 Two oceanic plates moving away from each other
  (diverging)
 The ocean floors move like conveyor belts,
  moving the continents away from each other
 New crust is formed where the plates are
  spreading
SEA FLOOR SPREADING AND PLATE
TECTONICS
   Convection currents is the engine that drives the
    plates to move
TYPES OF PLATE BOUNDARIES
 Convergent
 Divergent

 Transform
WHAT HAPPENS WHEN PLATES
COLLIDE?
 Oceanic/Oceanic- the older plate (more dense
  plate) will subduct
 Oceanic/Continental- oceanic plate subducts
  because it is more dense
 Continental/Continental- forms mountain ranges
DEFORMATIONS CAUSED BY
STRESS
 Anticlines
 Synclines

 Plateaus
TYPES OF FAULTS
 Strike- Slip Fault
 Reverse Fault

 Normal Fault
FOCUS AND EPICENTER
 Focus- point BENEATH Earth’s surface where
  rock under stress breaks to cause an earthquake
 Epicenter- point on the surface directly above the
  focus
SEISMIC WAVES
 P Waves- compress and expand the ground like
  an accordion (happen first)
 S Waves- vibrate from side to side and up and
  down
 Surface Waves- when waves reach the surface
  (cause most damage)
SCALES FOR MEASURING
EARTHQUAKES
 Mercalli Scale- rates earthquakes based on
  damage
 Richter Scale

 Moment Magnitude scale
RISK FACTORS FOR EARTHQUAKES
 Shaking
 Liquefaction

 Aftershocks

 Tsunamis
DEVICES TO MONITOR AND DETECT
EARTHQUAKES
   tiltmeter
WHERE DO VOLCANOES FORM?
 Convergent boundaries
 Divergent boundaries

 Hot spots
TYPES OF VOLCANOES
 Composite
 Shield

 Cinder cone
PARTS OF A VOLCANO
ACTIVITY OF VOLCANOES
 Active
 Dormant

 Extinct
MAGMA AND LAVA
 Magma is molten rock under the ground
 When magma reaches the Earth’s surface, it is
  called lava
SILICA AND MAGMA’S VISCOSITY
 Silica determines viscosity
 The more silica, the more viscous a substance is

 More silica magma is light colored and is too
  sticky to flow far
 Less silica magma flows readily and produces
  dark colored lava
HOW DOES TRAPPED GAS EFFECT A
VOLCANO’S ERUPTION?
   As magma rises toward the surface, the pressure
    decreases and the dissolved gases begin to expand and
    exert an enormous force

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Earth Science Review: Constructive vs Destructive Forces and Plate Tectonics

  • 2. DIFFERENCE BETWEEN CONSTRUCTIVE AND DESTRUCTIVE FORCES  Constructive forces build up the earth’s surface  Destructive wear away earth’s surface
  • 3. LAYERS OF EARTH  Lithosphere- consists of crust and top of mantle  Separates into plates  Meets at plate boundaries  Asthenosphere- located under lithosphere; what the lithosphere glides on top of
  • 4. PANGEA  All the continents were once joined together in a super continent  Continents fit together like puzzle pieces
  • 5. SEA FLOOR SPREADING  Two oceanic plates moving away from each other (diverging)  The ocean floors move like conveyor belts, moving the continents away from each other  New crust is formed where the plates are spreading
  • 6. SEA FLOOR SPREADING AND PLATE TECTONICS  Convection currents is the engine that drives the plates to move
  • 7. TYPES OF PLATE BOUNDARIES  Convergent  Divergent  Transform
  • 8.
  • 9. WHAT HAPPENS WHEN PLATES COLLIDE?  Oceanic/Oceanic- the older plate (more dense plate) will subduct  Oceanic/Continental- oceanic plate subducts because it is more dense  Continental/Continental- forms mountain ranges
  • 10. DEFORMATIONS CAUSED BY STRESS  Anticlines  Synclines  Plateaus
  • 11. TYPES OF FAULTS  Strike- Slip Fault  Reverse Fault  Normal Fault
  • 12. FOCUS AND EPICENTER  Focus- point BENEATH Earth’s surface where rock under stress breaks to cause an earthquake  Epicenter- point on the surface directly above the focus
  • 13. SEISMIC WAVES  P Waves- compress and expand the ground like an accordion (happen first)  S Waves- vibrate from side to side and up and down  Surface Waves- when waves reach the surface (cause most damage)
  • 14. SCALES FOR MEASURING EARTHQUAKES  Mercalli Scale- rates earthquakes based on damage  Richter Scale  Moment Magnitude scale
  • 15. RISK FACTORS FOR EARTHQUAKES  Shaking  Liquefaction  Aftershocks  Tsunamis
  • 16. DEVICES TO MONITOR AND DETECT EARTHQUAKES  tiltmeter
  • 17. WHERE DO VOLCANOES FORM?  Convergent boundaries  Divergent boundaries  Hot spots
  • 18. TYPES OF VOLCANOES  Composite  Shield  Cinder cone
  • 19. PARTS OF A VOLCANO
  • 20. ACTIVITY OF VOLCANOES  Active  Dormant  Extinct
  • 21. MAGMA AND LAVA  Magma is molten rock under the ground  When magma reaches the Earth’s surface, it is called lava
  • 22. SILICA AND MAGMA’S VISCOSITY  Silica determines viscosity  The more silica, the more viscous a substance is  More silica magma is light colored and is too sticky to flow far  Less silica magma flows readily and produces dark colored lava
  • 23. HOW DOES TRAPPED GAS EFFECT A VOLCANO’S ERUPTION?  As magma rises toward the surface, the pressure decreases and the dissolved gases begin to expand and exert an enormous force