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Crustal movements may cause layers of rocks to be folded.

Compressional forces in the crust push toward each other in opposite directions, bending and folding the rock layers in various ways.

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Types of Fold

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Simple or Symmetrical Fold simple.PSD (48666 bytes)

equal steepness
2 forces are of equal strength

Asymmetrical Fold            assymetrical.PSD (43679 bytes)

one limb is steeper than the other  
1 force is slightly greater than the other

Overturned Fold     turned.PSD (31942 bytes)

one limb pushes over the other 
opposing force is greater

 

Faulting

-a fracture or break in the earth's crust along a line of weakness

Faulting may be caused either tensional or Compressional forces exerted on rocks either laterally or vertically.

  ----> compressional <------                          <------- tensional----------->

3 major types of Faulting

Normal Faults     ---> caused by tension pulling the crust apart

Reverse Faults    ---> caused by compressional forces in the Earth's crust

Tear Faults        ---> caused by adjacent sections of the crust sliding past each                                  other  horizontally   e.g.  San Andreas Fault in California                                     USA

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BLOCK MOUNTAIN (HORST)

~ formed when faulting in the crust due to either tension or compression causes a block of the crust to be uplifted, relative to the depressed crust on either side of it.

A block mountain  with a horizontal surface is called a horst. It has 2 pronounced scarps or either called 'overhanging cliff'.

RIFT VALLEY (GRABEN)

~ A rift valley or graben is a long valley, formed by the sinking of land between two roughly parallel faults. e.g. East African Rift Valley

It may be due to tension or compression.

Normal Fault        ~ results in vertical displacement of rocks

Reverse Fault       ~ results in vertical displacement of rocks

Tear Fault            ~ results in horizontal displacement of rocks

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