glacial dating- visualizing in 3D Flashcards

1
Q

Why do rocks fold and fault?

A
  • when rocks are subjected to stress and undergo strain they fold and fault
  • there are different kinds oof stress including compressional, tensoinal, and shear
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2
Q

How do rocks respond to stress?

A
  • rocks respond in two ways:
  • Elastic strain: deformed body recovers when stress is removed. Think elastic band. When the stress is beyond the elastic limit, permanent deformation is caused
  • Plastic strain: bends but does not return to original shape. Rocks under increased temperature/pressure. For example, rocks in the mantle. Ex. glacial ice, asthenosphere
  • brittle
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3
Q

*How do rocks fold?

A
  • folds or bends in layered rocks. caused by plastic strain
  • depending on the stress, strain behaviour on the rock changes. Folds can become permanent after strain is removed: this can casued a fault
  • types of folds: anticline, syncline, overturned, recumbent
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4
Q

What are fractures and faults?

A

joints- rocks fractures, no displacement (not a fault)
faults- fractures along which movements has taken place. An active fault is classified as having movement within 11000 years
- Types of faults: normal, reverse, thrust, strike slip

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5
Q

How does fault formation reflect the type of stress to which rocks are subjected?*****

A
  • different types of faults are caused by different types of stress
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6
Q

anticline

A
  • upward arching fold
  • synclines and anticlines often occur together
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7
Q

syncline

A
  • downward arching fold
  • synclines and anticlines often occur together
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8
Q

overturned fold

A

anticline goes over syncline due to lots of folding

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9
Q

recumbent fold

A
  • axial plane is at the axsis of orientation. straight lines in the horizion
  • axial plane is essentially horizontal,
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10
Q

compressional stress

A
  • forces pushing together
  • convergent boundaries have compressional stress
  • ex. convergent plate margins
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11
Q

tensional stress

A
  • forces pulling apart
  • ex. divergent plant margins
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12
Q

shear stress

A
  • parallel; opposing forces
  • ex. transform plate margins
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13
Q

normal fault

A
  • hanging wall block moves downward relative to footwall block
  • caused by tensional stress
  • can produce a graben or horst
  • ex. East african rift valley, or just a rift valley in general
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14
Q

reverse fault

A
  • hanging wall block moves upwards relative to footwall block
  • causes by compressional stress
  • often caused by compressional stress
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15
Q

thrust fault

A
  • reverse fault with very low angle fault (less than 45 degrees)
  • causes by compressional stress
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16
Q

strike slip fault

A
  • a fault where the movement is predominantly horizontal and therefore parallel to the strike of the fault
  • causes by shear stress
  • found in transform boundaries
17
Q

hanging wall block

A
  • overlies an inclined fault plane
18
Q

footwall block

A
  • underlies an incline fault plane
19
Q

strain

A

change in size/shape in response to stress

20
Q

folds

A
  • bends in layered rock due to plastic strain
21
Q

hinge line

A

axis of the fold

22
Q

axial plane

A

plane contaiing all hinge lines of a fold

23
Q

where do we find water/gas/oil?

A
  • we can map out where faults may be
  • most fossil fuels are found in sedimentary rock
  • reasources can be found in a resivor over an anticline trap, oil and gas rise to the crest(top) of the fold
  • also found in fault traps which is where oil and gas collect in tilted strata adjacent to the fault
  • also salt dome traps and stratigraphic trap
  • it takes millions of years for reasoureces to replenish
  • it is important because we are buring fossil fuels so quickly that they will not be replenished in our lifetime
24
Q

horst

A

a block pushed upward relative to the blocks on either side b the faulting

25
Q

graben

A

a block that has been lowered relative to the blocks on either side due to the faulting

26
Q

brittle

A
  • breaks or fractures, ex. faults
  • surface rocks
27
Q

appalacian valley and ridge

A
  • folding at appalacians tells us that appalacians are no longer growing
  • it is an old mountain range
  • folds are only found at active tctonic plate boundaries
  • at the appalacians, it is no lonher active and is eroding away