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STRESSES,
FOLDS and
FAULTS
STRESS
 the force applied to a rock that causes deformation
TYPES OF STRESS
Tension
Compression
Shear
TENSION
 force that pulls on crust in opposite
direction
 causes crust to stretch and become thin in
middle
COMPRESSION
 force that pushes rock in together
 causes crust to rise
SHEAR
 force that pushes rock in 2 opposite
directions
 causes masses of rock to break, slip, or
change shape
FOLD
 a bend in rock that is the response to
compressional forces.
 most visible in rocks that contain
layering.
TYPES OF FOLD
Monocline
Syncline
Anticline
MONOCLINE
 involves a slight bend in otherwise parallel layers of
rock.
 form by vertical movement and generally found fault
below monocline
ANTICLINE
 a fold that arches upward. The rocks dip away from
the center of the fold.
 The oldest rocks are found at the center. The
youngest rocks are draped over them at the top of
the structure
 Also called the “dome”.
SYNCLINE
 a fold where the rock layers are warped downward.
Both anticlines and synclines are the result of
compressional stress.
 the youngest rocks are at the center. The oldest
rocks are at the outside edges.
 Also called the “basin”.
FAULT
 are cracks in the earth's crust where
movement occurs on at least one side.
 are formed in the Earth's crust as brittle
response to STRESS.
 Earthquakes occur along faults because of
the sliding
PARTS OF A FAULT
TYPES OF FAULT
 Normal Fault
 Reverse Fault
 Strike-Slip Fault
NORMAL FAULT
 happen in areas where the rocks are pulling
apart (tension stress) so that the rocky crust of
an area is able to take up more space.
REVERSE FAULT
 the rocks are pushed together (compression stress),
and the hanging wall moves upward along the fault
relative to the footwall.
 This is literally the 'reverse' of a normal fault.
 Sometimes called “Thrust fault”
STRIKE – SLIP FAULT
 a fault on which the two blocks slide past
one another caused by shearing stress.

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STRESSES, FOLDS AND FAULTS.pptx

  • 2. STRESS  the force applied to a rock that causes deformation
  • 4. TENSION  force that pulls on crust in opposite direction  causes crust to stretch and become thin in middle
  • 5. COMPRESSION  force that pushes rock in together  causes crust to rise
  • 6. SHEAR  force that pushes rock in 2 opposite directions  causes masses of rock to break, slip, or change shape
  • 7. FOLD  a bend in rock that is the response to compressional forces.  most visible in rocks that contain layering.
  • 9. MONOCLINE  involves a slight bend in otherwise parallel layers of rock.  form by vertical movement and generally found fault below monocline
  • 10. ANTICLINE  a fold that arches upward. The rocks dip away from the center of the fold.  The oldest rocks are found at the center. The youngest rocks are draped over them at the top of the structure  Also called the “dome”.
  • 11. SYNCLINE  a fold where the rock layers are warped downward. Both anticlines and synclines are the result of compressional stress.  the youngest rocks are at the center. The oldest rocks are at the outside edges.  Also called the “basin”.
  • 12. FAULT  are cracks in the earth's crust where movement occurs on at least one side.  are formed in the Earth's crust as brittle response to STRESS.  Earthquakes occur along faults because of the sliding
  • 13.
  • 14. PARTS OF A FAULT
  • 15. TYPES OF FAULT  Normal Fault  Reverse Fault  Strike-Slip Fault
  • 16.
  • 17. NORMAL FAULT  happen in areas where the rocks are pulling apart (tension stress) so that the rocky crust of an area is able to take up more space.
  • 18. REVERSE FAULT  the rocks are pushed together (compression stress), and the hanging wall moves upward along the fault relative to the footwall.  This is literally the 'reverse' of a normal fault.  Sometimes called “Thrust fault”
  • 19.
  • 20. STRIKE – SLIP FAULT  a fault on which the two blocks slide past one another caused by shearing stress.