Tectonic Processes and Hazards

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COLLISION ZONES + TRANSFORM ZONES

Collision Zones:

  • e.g. Himalayas
  • two continental crusts come together, same low density so no subduction
  • plates fold and 'crumple' together causing mountains

Transform Zones:

  • conservative plate boundaries
  • faults 'join up' 
  • tension builts up then a 'jolt' causes earthquakes
  • NO VOLCANO
  • shallow focal depth so hihg-magnitudes, can be very destructive 
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