Eduqas GCSE Geology · 1.5

Deformational Structures

50 revision questions with answers for 1.5 Deformational Structures in Eduqas GCSE Geology (spec C480QS). Practise with flashcards, a topic quiz, a random quiz across the course, 5 crosswords, Five Degrees, Associations, or read every question and answer below. Not official Eduqas material.

All 50 questions and answers

  1. Question 1

    What is tectonic stress?

    Answer:
    A force per unit area acting on rock that may cause it to deform.
  2. Question 2

    What does compressional stress do to rocks?

    Answer:
    It squeezes them, commonly shortening and folding them or producing reverse faults.
  3. Question 3

    What does tensional stress do to rocks?

    Answer:
    It pulls them apart, commonly extending the crust and producing normal faults.
  4. Question 4

    What does shear stress do?

    Answer:
    It pushes adjacent parts in opposite directions, commonly producing sideways displacement.
  5. Question 5

    Why can rocks fold rather than fracture?

    Answer:
    Under suitable pressure, temperature and timescale, rocks can deform ductilely.
  6. Question 6

    What is strike?

    Answer:
    The compass direction of a horizontal line on an inclined planar surface.
  7. Question 7

    What is dip?

    Answer:
    The maximum angle at which a planar surface slopes from the horizontal, and the direction of that slope.
  8. Question 8

    How are strike and dip direction related?

    Answer:
    Dip direction is at right angles to the strike direction.
  9. Question 9

    A bed strikes north-south and dips east. What is the dip direction in degrees?

    Answer:
    090 degrees, measured clockwise from north.
  10. Question 10

    What instrument is used to measure dip in the field?

    Answer:
    A compass-clinometer.
  11. Question 11

    What does a dip of zero degrees mean?

    Answer:
    The measured plane is horizontal.
  12. Question 12

    Can a vertical bed have a dip angle of 90 degrees?

    Answer:
    Yes. A vertical plane dips at 90 degrees.
  13. Question 13

    Why may a field dip measurement be unreliable?

    Answer:
    The exposed surface may be uneven, weathered, too small or not the true bedding plane.
  14. Question 14

    How can you improve a dip measurement on an uneven surface?

    Answer:
    Find a representative bedding surface, use a flat board if appropriate, and repeat readings at several points.
  15. Question 15

    Why should a geological map show both dip direction and angle?

    Answer:
    The two together describe how steeply and in which direction the bed slopes.
  16. Question 16

    What is a fold?

    Answer:
    A bend in originally more nearly planar rock layers caused by deformation.
  17. Question 17

    What is an antiform?

    Answer:
    A fold that is convex upwards, with limbs dipping away from the hinge in a simple upright fold.
  18. Question 18

    What is a synform?

    Answer:
    A fold that is concave upwards, with limbs dipping towards the hinge in a simple upright fold.
  19. Question 19

    What is the limb of a fold?

    Answer:
    One side of the fold between adjacent hinges.
  20. Question 20

    What is an axial plane?

    Answer:
    An imaginary plane joining the hinge lines of successive folded layers.
  21. Question 21

    What is an axial plane trace on a map?

    Answer:
    The line where the axial plane intersects the mapped surface.
  22. Question 22

    A fold has unequal limb dips. How should it be described?

    Answer:
    It is asymmetrical; state the dip on each limb if measurements are given.
  23. Question 23

    Why should a field sketch preserve the number of visible beds?

    Answer:
    Bed number and geometry are evidence for interpreting the fold and its history.
  24. Question 24

    What should be included in a useful fold sketch?

    Answer:
    Accurate curved bed outlines, limb dips, a scale and labels for the relevant structures.
  25. Question 25

    Can a synform or antiform name alone tell you the age order of beds?

    Answer:
    No. These names describe shape; age order needs separate evidence.
  26. Question 26

    What is a fault?

    Answer:
    A fracture in rock along which displacement has occurred.
  27. Question 27

    What is fault displacement?

    Answer:
    The amount and direction of movement of markers or rock across a fault.
  28. Question 28

    What is a normal fault?

    Answer:
    A fault in which the hanging wall moves down relative to the footwall, commonly under tension.
  29. Question 29

    What is a reverse fault?

    Answer:
    A fault in which the hanging wall moves up relative to the footwall, commonly under compression.
  30. Question 30

    What is a thrust fault?

    Answer:
    A low-angle reverse fault in which the hanging wall has moved up relative to the footwall.
  31. Question 31

    What is a strike-slip fault?

    Answer:
    A fault where displacement is mainly horizontal, parallel to the fault's strike.
  32. Question 32

    Which stress commonly produces a normal fault?

    Answer:
    Tensional stress.
  33. Question 33

    Which stress commonly produces a reverse fault?

    Answer:
    Compressional stress.
  34. Question 34

    Which stress commonly produces a strike-slip fault?

    Answer:
    Shear stress.
  35. Question 35

    How can matching beds help identify a fault?

    Answer:
    A bed or contact offset across a fracture provides a marker showing displacement.
  36. Question 36

    A marker bed is offset horizontally across a fault on a map. What type is suggested?

    Answer:
    Strike-slip, provided the evidence shows predominantly horizontal movement.
  37. Question 37

    How do you identify the hanging wall on an inclined fault?

    Answer:
    It is the block above the fault plane; the footwall lies below it.
  38. Question 38

    Why is identifying the downthrown block alone not always enough to name a fault?

    Answer:
    The orientation of the fault plane and relative movement of hanging wall and footwall are also needed.
  39. Question 39

    A mapped contact is offset 3 cm on a 1:10,000 map. What is the real offset?

    Answer:
    3 cm x 10,000 = 30,000 cm = 300 m.
  40. Question 40

    What is an unconformity?

    Answer:
    A surface representing a gap in the geological record caused by erosion and/or non-deposition.
  41. Question 41

    What is an angular unconformity?

    Answer:
    A surface where younger beds overlie eroded older beds with a different orientation.
  42. Question 42

    Order events for an angular unconformity.

    Answer:
    Older beds deposit, deform and uplift; erosion truncates them; younger sediment is deposited above.
  43. Question 43

    What visual evidence supports an angular unconformity?

    Answer:
    Older inclined or folded beds are truncated beneath younger beds at a different angle.
  44. Question 44

    Why does an unconformity represent missing time?

    Answer:
    Some rock was eroded or no sediment accumulated during part of the sequence.
  45. Question 45

    Are younger beds below or above an undisturbed unconformity?

    Answer:
    Above it; the older rocks lie beneath the erosional surface.
  46. Question 46

    Why should you record a grid reference for an exposure?

    Answer:
    It lets the observation be accurately located on a map and revisited.
  47. Question 47

    Give two hazards to consider at a cliff exposure.

    Answer:
    Falling rock and rising tides; also assess ground stability and safe access.
  48. Question 48

    What should a field sketch of a fault include?

    Answer:
    The fault trace, matching offset beds, relative displacement, a scale and clear labels.
  49. Question 49

    Why record several structural readings rather than just one?

    Answer:
    Repeated readings show variation, help identify errors and strengthen the interpretation.
  50. Question 50

    How can cross-sections assist geological interpretation?

    Answer:
    They show an inferred vertical slice through beds and structures, linking map observations in three dimensions.

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