Earthquakes: Plate Boundaries

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The Tectonic Plates

  • Pacific Plate
  • North American Plate
  • South American Plate
  • Nazca Plate
  • Antarctic Plate
  • African Plate 
  • Indian Plate 
  • Eurasian Plate
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Divergent/Constructive Margin

Two plates that are moving apart.

Example: Mid-Atlantic Ridge

  • Plates move away from each other 
  • Hot magma rises from beneath the ground
  • New mountains form under the sea
  • Mountain tops break the surface as volcanic islands
  • New crust is formed at the margin from cooling magma

The movemnet can cause earthquakes.

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Transform/Conservative Margin

Two plates sliding past each other.

Example: California San Andreas Fault

  • Plates try to slide past each other
  • Plates stick together/jam
  • Huge amounts of pressure build up
  • Pressure releases causing violent earthquake
  • No new crust is formed

This can cause earthquakes but not volcanic activity.

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Convergent/Collision Margin

Two plates moving towards each other, both continemtal crusts.

Example: Hamalayan Mountains

  • Plates move towards each other
  • Plates can't sink so crash into each other
  • Pressure causes the rocks to bend
  • Rocks pushed upwards to form mountains

The movement causes earthquakes but not volcanic activity.

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Convergent/Destructive Margin

Two plates that are moving towards each other.

Example: the Nazca Plate and the American Plate

  • Plates move towards each other
  • Heavier oceanic plate moves under continental plate
  • Plate rub together causing friction and severe earthquakes
  • Heat from mantle melts teh rock
  • Hot magma rises
  • Volcanic eruptions occur

Can cause earthquakes and volcanic activity.

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