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Plate boundaries compared

 Objective: To be able to draw a diagram,
   describe the features and explain the
processes occurring at each plate boundary
1) Describe the distribution of plate boundaries (3 marks)
2) Identify the type of plate boundary or boundaries found between:
a) The African and the Eurasian plate
b) The Indo Australian plate to the east of India and the Eurasian plate
c) The Eurasian plate and the North American plate
1 mark for each correct answer for question 2
Peer Assessment
• 1) The distribution of plate boundaries is very
  uneven (1 mark). However, they are often
  found on the edge of continents (1 mark) e.g.
  North and South American (1 mark) or in the
  middle of the ocean (1 mark) e.g. the mid
  Atlantic (1 mark).
• 2) (a) Destructive ( 1mark)
• (b) Collision zone (1 mark)
• (c) A constructive boundary (1 mark)
Plate Boundaries Compared




           Conservative margin
Conservative
                                                                                                  plate boundary




http://whs.moodledo.co.uk/file.php/1365/EarthSystems/Earth%20Systems/Transform%20faults%20in%20California%20and%20Turkey.swf
Plate Boundary and Explanation            Earthquakes      Volcanoes
Example

Conservative         •Plates slide past   High magnitude   • None
                     each other = Crust   earthquakes
San Andreas fault-   neither created or
North American       destroyed because
and Pacific plates   no magma or
(sliding past each   subduction
other in the same    •Friction between
direction)           plates = extreme
                     stress builds in
                     crustal rocks when
                     released =
                     earthquake
                     •Longer period of
                     movement = more
                     stress build up so
                     when released =
                     more energy
                     significant
                     earthquake
Constructive plate
          boundary


         f




http://www.youtube.com/watch?NR=1&v=t-ctk4KR-KU
http://www.youtube.com/watch?v=ep2_axAA9Mw&NR=1




 Destructive plate
    boundary
Collision
                                                                                              Zone




http://whs.moodledo.co.uk/file.php/1365/EarthSystems/Earth%20Systems/Collision%20Zones.swf
Tasks
• Complete the rest of the table using p14
  Purple Book and p14 Green Book
Plate Boundary     Explanation                    Earthquakes       Volcanoes
and Example

Constructive       •New basaltic material rises   • Low magnitude   Shield Volcanoes not
                   to the surface forcing         earthquakes       very explosive or
•Iceland on the    oceanic plates apart           maximum 6 on      dangerous
mid-Atlantic       •Hot magma is able to fill     Richter Scale     Erupt basic lava and
ridge the          the “gap” creating new                           occur in fissures
Eurasian and       crust.                                           (cracks in the crust)
North American •As magma continues to
plates are pulling build up new mountain
apart              ranges form under sea =
                   mid-ocean ridge
                   •Magma continues to rise
                   until eventually above sea =
                   volcanic island
Plate Boundary and   Explanation           Earthquakes           Volcanoes
Example



Destructive          •Oceanic crust        The highest           Very explosive and
                     destroyed             magnitude             dangerous
Andes Mountains in   •Oceanic plate        earthquakes           volcanoes with
Peru and Chiles      subducts under less   recorded occur here   steep sides called
where Nazca          dense continental                           composite cone
oceanic plate is     plate forming fold                          volcanoes
subducted under      mountains in the                            Erupt andesitic lava
the continental      process
South American       •Magma rises
plate                through weaknesses
                     melting crust
                     forming volcanoes
Plate boundary and    •Processes         Earthquakes   Volcanoes
Example



Collision Zone        •Two continental     Very high   None because no
                      plates moving        magnitude   material is
Himalayas             towards each other earthquakes   subducted
Indian and Eurasian   •Same density so no
continental plate     subduction occurs
crash into each       this cause the crust
other                 to buckle and fold
                      creating fold
                      mountains
                      • No volcanoes
                      occur here as
                      subduction does not
                      occur
                      •Crust neither
                      formed or
                      destroyed

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L3 plate boundaries

  • 1. Plate boundaries compared Objective: To be able to draw a diagram, describe the features and explain the processes occurring at each plate boundary
  • 2. 1) Describe the distribution of plate boundaries (3 marks) 2) Identify the type of plate boundary or boundaries found between: a) The African and the Eurasian plate b) The Indo Australian plate to the east of India and the Eurasian plate c) The Eurasian plate and the North American plate 1 mark for each correct answer for question 2
  • 3. Peer Assessment • 1) The distribution of plate boundaries is very uneven (1 mark). However, they are often found on the edge of continents (1 mark) e.g. North and South American (1 mark) or in the middle of the ocean (1 mark) e.g. the mid Atlantic (1 mark). • 2) (a) Destructive ( 1mark) • (b) Collision zone (1 mark) • (c) A constructive boundary (1 mark)
  • 4. Plate Boundaries Compared Conservative margin
  • 5. Conservative plate boundary http://whs.moodledo.co.uk/file.php/1365/EarthSystems/Earth%20Systems/Transform%20faults%20in%20California%20and%20Turkey.swf
  • 6. Plate Boundary and Explanation Earthquakes Volcanoes Example Conservative •Plates slide past High magnitude • None each other = Crust earthquakes San Andreas fault- neither created or North American destroyed because and Pacific plates no magma or (sliding past each subduction other in the same •Friction between direction) plates = extreme stress builds in crustal rocks when released = earthquake •Longer period of movement = more stress build up so when released = more energy significant earthquake
  • 7. Constructive plate boundary f http://www.youtube.com/watch?NR=1&v=t-ctk4KR-KU
  • 9. Collision Zone http://whs.moodledo.co.uk/file.php/1365/EarthSystems/Earth%20Systems/Collision%20Zones.swf
  • 10. Tasks • Complete the rest of the table using p14 Purple Book and p14 Green Book
  • 11. Plate Boundary Explanation Earthquakes Volcanoes and Example Constructive •New basaltic material rises • Low magnitude Shield Volcanoes not to the surface forcing earthquakes very explosive or •Iceland on the oceanic plates apart maximum 6 on dangerous mid-Atlantic •Hot magma is able to fill Richter Scale Erupt basic lava and ridge the the “gap” creating new occur in fissures Eurasian and crust. (cracks in the crust) North American •As magma continues to plates are pulling build up new mountain apart ranges form under sea = mid-ocean ridge •Magma continues to rise until eventually above sea = volcanic island
  • 12. Plate Boundary and Explanation Earthquakes Volcanoes Example Destructive •Oceanic crust The highest Very explosive and destroyed magnitude dangerous Andes Mountains in •Oceanic plate earthquakes volcanoes with Peru and Chiles subducts under less recorded occur here steep sides called where Nazca dense continental composite cone oceanic plate is plate forming fold volcanoes subducted under mountains in the Erupt andesitic lava the continental process South American •Magma rises plate through weaknesses melting crust forming volcanoes
  • 13. Plate boundary and •Processes Earthquakes Volcanoes Example Collision Zone •Two continental Very high None because no plates moving magnitude material is Himalayas towards each other earthquakes subducted Indian and Eurasian •Same density so no continental plate subduction occurs crash into each this cause the crust other to buckle and fold creating fold mountains • No volcanoes occur here as subduction does not occur •Crust neither formed or destroyed