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Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
Earthquakes(Varidhi & Vidhya)
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Earthquakes(Varidhi & Vidhya)

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  • 1.  
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  • 4.  
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  • 8.  
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  • 12. <ul><li>The earths outermost surface is broken into 12 rigid plates which are 60-200 km thick. </li></ul>
  • 13. Plate Boundaries
  • 14. &nbsp;
  • 15. <ul><li>THE SAN ANDREAS FAULT </li></ul>
  • 16. Strike-Slip Thrust Normal
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  • 33. Turnagain Heights, Alaska,1964 (upper left inset); Santa Cruz Mtns, California , 1989
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  • 35. &nbsp;
  • 36. No!
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