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Chapter 9 Plate tectonics
An Idea Before Its Time   ,[object Object],[object Object],[object Object],[object Object]
Evidence: The Continental Puzzle ,[object Object],[object Object],[object Object]
 
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Evidence for Continental Drift
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[object Object],[object Object],[object Object],[object Object]
 
[object Object],[object Object],[object Object]
 
[object Object],[object Object]
 
[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Types of Plate Boundaries   ,[object Object],[object Object],[object Object]
 
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[object Object],[object Object]
 
[object Object],[object Object],[object Object]
Actions at Plate Boundaries   ,[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
 
[object Object],[object Object]
 
[object Object],[object Object],[object Object]
 
[object Object],[object Object],[object Object]
 
Evidence of hot spot rifting ,[object Object],[object Object],[object Object],[object Object],[object Object]
How are plates broken ????? ,[object Object]
If Hot Spots Connect….. ,[object Object],Failed arms  do not connect
Failed Arms Become ……………. ,[object Object]
 
 
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[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object]
 
[object Object],[object Object],[object Object],[object Object]
 
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Testing Plate Tectonics   ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object]
 
 
[object Object],[object Object],[object Object],[object Object]
 
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[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
 
Mechanics of Plate Motion   ,[object Object],[object Object]
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[object Object],[object Object]
 
 
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Beginning 4 billion years ago with small volcanic chains (arcs), created by convection cells and subduction zones that evolved into proto-continents through many individual subduction zones     
When the proto-continents collided micro-continents were created that evolved into the major continents today (such as North and South America, Siberia, Australia).

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Chapter 9outline