Types of plate boundaries

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  • Created by: Sue.Kandi
  • Created on: 20-05-17 14:12

Destructive plate boundaries

  • A destructive plate boundary is sometimes called a convergent or tensional plate margin
  •  This occurs when oceanic and continental plates move together
  • The oceanic plate is forced under the lighter continental plate.
  • Friction causes melting of the oceanic plate and may trigger earthquakes.
  • Magma rises up through cracks and erupts onto the surface.
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Constructive plate boundaries

  • A constructive plate boundary, sometimes called a divergent plate margin, occurs when plates move apart.
  • Volcanoes are formed as magma wells up to fill the gap, and eventually new crust is formed.
  • This pulls the crust apart and creates fissures and faults which molten magma can reach the surface.
  • Can form islands.
  • E.g. mid-Atlantic Ridge.
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Collision plate boundaries

  • Collision zones form when two continental plates move towards each other.
  • Neither plate is forced under the other, so both are forced up and form fold mountains.
  • E.g. Indo-Australian Plate & Eurasian Plate.
  • The buckling has led to the formation of the world's biggest mountain range, the Himalayanchain & the Tibetan plateau to the north of it
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Conservative plate boundaries

  • A conservative plate boundary is sometimes called a transform plate margins.
  • Occurs where plates slide past each other in opposite directionsin the same direction but at different speeds.
  • Friction is eventually overcome and the plates slip past in a sudden movement.
  • The shockwaves created produce an earthquake.
  • E.g San Andreas Fault in California. 
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