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DIASTROPHISM –FOLDING,
AND FAULTING
FORCES OF PRESSURE THAT
SHAPE THE EARTH’S SURFACE
•Diastrophism – deformation
of the Earth’s crust.
• Folding – bending of solid rock
due
to compressional forces over
a
long period of time.
• Faulting – breaking of solid rock
FOLD
Anticline and Syncline
•Another type of fold
is molocline
•Monocline is a
simple bend in the
rock layers so that
they are no longer
RECUMBENT FOLD
•Recumbent fold has an
essentially horizontal
axial plane. linear, fold
axial plane oriented at
low angle resulting in
overturned strata in one
limb of the fold.
CHEVRON FOLD
•Chevron folds are a
structural feature
characterized by
repeated well behaved
folded beds with straight
limbs and sharp hinges.
ISOCLINAL FOLD
• Isoclinal folds are similar to
symmetrical folds, but these folds
both have the same angle and are
parallel to each other.
• 'Iso' means 'the same' (symmetrical),
and 'cline' means 'angle,' so this
name literally means 'same angle.’
• So isoclinal folds are both
symmetrical and aligned in a parallel
fashion.
FAULT
FORCES THAT SHAPE THE
EARTH’S SURFACE
• There are three main types of forces of
pressure that work to shape (and re-shape)
the Earth’s surface:
–Compression forces (‘squeezing’)
–Extension (or tension) forces (‘stretching’)
–Shearing forces (‘ripping’)
FORCES
NORMAL FAULTS: DIP SLIP
FAULTS
• Normal faults are the result of tensional (or
extensional) forces acting to pull apart the
surface.
• The hanging wall drops relative to the
footwall.
• Normal faults can occur across vast areas
due to lithospheric stretching.
– Basin and Range in Western USA
NORMAL FAULT: DIP SLIP
Hanging wall
Footwall
Tension forces
Tension forces
REVERSE FAULT – DIP SLIP
• Reverse faults are the result of
compression forces
• The footwall drops relative to the hanging
wall
Reverse Fault – Dip Slip
Footwall
Hanging wall
TRANSFORM FAULTS:
SHEARING FORCES
• Transform faults can be found at plate
boundaries as one plate slides horizontally
past another.
– Strike-slip faults
• Most transform faults are found on the
ocean floor as part of the active offset
along divergent plate boundaries.
TRANSFORM FAULTS: PLATE
BOUNDARIES
• At plate boundaries, when two tectonic
plates grind past each other, there is
usually no volcanism or mountain building
occurring.
• One of the largest transform faults in the
world is the San Andreas Fault
– Separating the North American Plate from the
Pacific Plate in southern California.
TRANSFORM FAULTS: SAN ANDREAS
San Andreas Fault
San Andreas Fault in the
Carrizo Plain
View is looking south. Fault
is in the center of the folded
ridge area
CONSEQUENCES OF SAN
ANDREAS FAULT
• Along the San Andreas Fault, the Pacific plate slowly
grinds to the north.
• Los Angeles lies on the Pacific plate side of the fault,
while San Francisco is on the North American side.
– About 25 million years in the future, if movement continues in the
same direction, Los Angeles will be a suburb of San Francisco
(or vice versa)
• The San Andreas is a right-lateral transform fault, which
means that if you imagine standing on either side of the
fault and looking across to the opposite side, it seems to
you that the people and objects on the opposite side are
moving to your right.
•1. WHEN ROCKS BEND
DOWNWARD, THEY
FORM _______
•a. limbs
•b. syncline
•c. anticline
•d. cliff
•2. ROCKS UNDER
COMPRESSIONAL FORCE
ARE
•a. pushed apart
•b. transformed
•c. diverged
•d. crushed
•3. FAULTING OCCURS
DUE TO
•a. one force only
•b. two forces
•c. three
•d. four forces
•4. NORMAL FAULT IS
CAUSED BY
•a. tension
•b. compression
•c. expansion
•d. collision
•5. ROCKS UNDER
TENSIONAL FORCE ARE
•a. pushed towards each
other
•b. compressed
•c. expanded
•d. pulled apart
• 6. A FOLD MOUNTAIN IS A
TYPE OF LANDFORM THAT
IS CREATED WHEN TWO
CRUSTAL PLATES
• a. converge
• b. break
• c. diverge
• d. sink
•7. THERE ARE HOW
MANY TYPES OF FAULTS
•a. one
•b. two
•c. three
•d. four
• 8. CONVERSELY, A RIFT
VALLEY CAN BE FORMED
FROM A REVERSE FAULT
CAUSED BY
• a. tensional force
• b. compressional force
• c. expansion force
• d. contact force
•9. WHEN ROCKS BEND
UPWARD, THEY FORM
•a. monocline
•b. anticline
•c. syncline
•d. cliff
• 10. WHAT TYPE OF FORCE
IS INVOLVED IN THE
FORMATION OF
TRANSFORM FAULT?
• a. compressional force
• b. shearing force
• c. tensional force
• d. extension

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Lesson 7 DIASTROPHISM – FOLDING, FAULTING AND MORE.ppt

  • 1.
  • 2. DIASTROPHISM –FOLDING, AND FAULTING FORCES OF PRESSURE THAT SHAPE THE EARTH’S SURFACE
  • 3.
  • 4. •Diastrophism – deformation of the Earth’s crust. • Folding – bending of solid rock due to compressional forces over a long period of time. • Faulting – breaking of solid rock
  • 6.
  • 7.
  • 9. •Another type of fold is molocline •Monocline is a simple bend in the rock layers so that they are no longer
  • 10.
  • 12. •Recumbent fold has an essentially horizontal axial plane. linear, fold axial plane oriented at low angle resulting in overturned strata in one limb of the fold.
  • 14. •Chevron folds are a structural feature characterized by repeated well behaved folded beds with straight limbs and sharp hinges.
  • 16. • Isoclinal folds are similar to symmetrical folds, but these folds both have the same angle and are parallel to each other. • 'Iso' means 'the same' (symmetrical), and 'cline' means 'angle,' so this name literally means 'same angle.’ • So isoclinal folds are both symmetrical and aligned in a parallel fashion.
  • 17. FAULT
  • 18.
  • 19.
  • 20.
  • 21.
  • 22. FORCES THAT SHAPE THE EARTH’S SURFACE • There are three main types of forces of pressure that work to shape (and re-shape) the Earth’s surface: –Compression forces (‘squeezing’) –Extension (or tension) forces (‘stretching’) –Shearing forces (‘ripping’)
  • 24. NORMAL FAULTS: DIP SLIP FAULTS • Normal faults are the result of tensional (or extensional) forces acting to pull apart the surface. • The hanging wall drops relative to the footwall. • Normal faults can occur across vast areas due to lithospheric stretching. – Basin and Range in Western USA
  • 25. NORMAL FAULT: DIP SLIP Hanging wall Footwall Tension forces Tension forces
  • 26. REVERSE FAULT – DIP SLIP • Reverse faults are the result of compression forces • The footwall drops relative to the hanging wall
  • 27. Reverse Fault – Dip Slip Footwall Hanging wall
  • 28. TRANSFORM FAULTS: SHEARING FORCES • Transform faults can be found at plate boundaries as one plate slides horizontally past another. – Strike-slip faults • Most transform faults are found on the ocean floor as part of the active offset along divergent plate boundaries.
  • 29. TRANSFORM FAULTS: PLATE BOUNDARIES • At plate boundaries, when two tectonic plates grind past each other, there is usually no volcanism or mountain building occurring. • One of the largest transform faults in the world is the San Andreas Fault – Separating the North American Plate from the Pacific Plate in southern California.
  • 32. San Andreas Fault in the Carrizo Plain View is looking south. Fault is in the center of the folded ridge area
  • 33. CONSEQUENCES OF SAN ANDREAS FAULT • Along the San Andreas Fault, the Pacific plate slowly grinds to the north. • Los Angeles lies on the Pacific plate side of the fault, while San Francisco is on the North American side. – About 25 million years in the future, if movement continues in the same direction, Los Angeles will be a suburb of San Francisco (or vice versa) • The San Andreas is a right-lateral transform fault, which means that if you imagine standing on either side of the fault and looking across to the opposite side, it seems to you that the people and objects on the opposite side are moving to your right.
  • 34.
  • 35. •1. WHEN ROCKS BEND DOWNWARD, THEY FORM _______ •a. limbs •b. syncline •c. anticline •d. cliff
  • 36. •2. ROCKS UNDER COMPRESSIONAL FORCE ARE •a. pushed apart •b. transformed •c. diverged •d. crushed
  • 37. •3. FAULTING OCCURS DUE TO •a. one force only •b. two forces •c. three •d. four forces
  • 38. •4. NORMAL FAULT IS CAUSED BY •a. tension •b. compression •c. expansion •d. collision
  • 39. •5. ROCKS UNDER TENSIONAL FORCE ARE •a. pushed towards each other •b. compressed •c. expanded •d. pulled apart
  • 40. • 6. A FOLD MOUNTAIN IS A TYPE OF LANDFORM THAT IS CREATED WHEN TWO CRUSTAL PLATES • a. converge • b. break • c. diverge • d. sink
  • 41. •7. THERE ARE HOW MANY TYPES OF FAULTS •a. one •b. two •c. three •d. four
  • 42. • 8. CONVERSELY, A RIFT VALLEY CAN BE FORMED FROM A REVERSE FAULT CAUSED BY • a. tensional force • b. compressional force • c. expansion force • d. contact force
  • 43. •9. WHEN ROCKS BEND UPWARD, THEY FORM •a. monocline •b. anticline •c. syncline •d. cliff
  • 44. • 10. WHAT TYPE OF FORCE IS INVOLVED IN THE FORMATION OF TRANSFORM FAULT? • a. compressional force • b. shearing force • c. tensional force • d. extension