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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.
Types of Fold
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
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.
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