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FOLDING & FAULTING
FOLDING
●WHEN EARTH’S CRUST BENDS, FOLD
OCCUR
●FOLDING OCCURS UNDER
COMPRESSION WHEN FORCES ACT
TOWARDS EACH OTHER, SUCH AS
WHEN PLATES COLLIDE.
DEFINITIONS
▪COMPRESSION
-reducing it in volume by pressing it together
▪TENSION
-To cause an extension of a body or to restore the
shape of an extended elastic object
PART OF A FOLD:
-Layers of rocks of continental crust
-2 slides of a fold are called the climbs.
-fold mountain & synclines from valley
THERE ARE 2 MAIN FOLD MOUNTAIN
SYSTEM IN THE WORLD:
A.) The old Caledonian fold mountain
B.) The Circum-pacific region surrounding the
specific ocean
FAULTING
BLOCK MOUNTAIN OR HORSTBLOCK
MOUNTAIN OR HORST
-Block that raised between 2 parallel faults
-A horst can also be formed by sinking of block
RIFT VALLEY OR GRABEN
-Is formed when block between 2 parallel faults sinks
or when block on either side of 2 parallel faults are
thrust up over central block.
-eggs are the rift valley & the east African rift valley.

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Folding & faulting

  • 2. FOLDING ●WHEN EARTH’S CRUST BENDS, FOLD OCCUR ●FOLDING OCCURS UNDER COMPRESSION WHEN FORCES ACT TOWARDS EACH OTHER, SUCH AS WHEN PLATES COLLIDE.
  • 3. DEFINITIONS ▪COMPRESSION -reducing it in volume by pressing it together ▪TENSION -To cause an extension of a body or to restore the shape of an extended elastic object
  • 4. PART OF A FOLD: -Layers of rocks of continental crust -2 slides of a fold are called the climbs. -fold mountain & synclines from valley
  • 5. THERE ARE 2 MAIN FOLD MOUNTAIN SYSTEM IN THE WORLD: A.) The old Caledonian fold mountain B.) The Circum-pacific region surrounding the specific ocean
  • 6. FAULTING BLOCK MOUNTAIN OR HORSTBLOCK MOUNTAIN OR HORST -Block that raised between 2 parallel faults -A horst can also be formed by sinking of block RIFT VALLEY OR GRABEN -Is formed when block between 2 parallel faults sinks or when block on either side of 2 parallel faults are thrust up over central block. -eggs are the rift valley & the east African rift valley.