Quiz over Chapter 10 Flashcards

(41 cards)

1
Q

Deformation

A

refers to all changes in the shape or position of a rock body in response to stress

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2
Q

Rock or geologic Structures

A

features that result from forces generated by the interactions of tectonic plates
(includes folds, faults, and joints)

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3
Q

Stress

A

the force that deforms rocks

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4
Q

Magnitude

A

a function of the amount of force applied to a given area

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5
Q

When stresses on a rock exceed its strength….

A

the rock deforms by flowing, folding, fracturing, or faulting

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6
Q

Confining pressure

A

stress applied to uniformity in all directions

squeezes rocks, making them stronger and harder to break

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7
Q

differential stress

A

Stress applied unequally in different directions

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8
Q

Types of Stress

A

Compressional
Tensional
Shear

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9
Q

Compressional Stress

A

squeezes a rock and shortens a rock body

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10
Q

tensional stress

A

pulls apart a rock unit and lengthens it

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11
Q

Shear stress

A

Produces a motion similar to slippage that occurs between individual playing cards when the top of the stack is moved relative to the bottom

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12
Q

Strain

A

change in shape of a rock caused by differential stress

strained bodies lose their original configuration during deformation

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13
Q

Elastic deformation

A

rock returns to nearly its original size and shape when the stress is removed

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14
Q

ductile deformation

A

bends

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15
Q

brittle deformation

A

breaks

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16
Q

Temperature

A

Higher temp deform by ductile deformation {deep}

Cooler rocks form by brittle deformation {on surface or high up in crust}

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17
Q

Factors that affect rock strength

A

Rock type
Time
Temperature
Pressure

18
Q

Rock type

A

Crystalline igneous rocks generally experience brittle deformation, whereas sedimentary and metamorphic rocks experience ductile deformation

19
Q

Time

A

forces applied over a long period of time generally result in ductile deformation

20
Q

Joints

A

cracks in the rocks resulting from the rock being stretched and pulled apart
created columns

21
Q

Faults

A

fractures in the rocks where rocks on one side of the fault are displaced relative to the rocks on the other side of the fault

22
Q

Folds are evidence

A

that rocks can bend without breaking

result of deformation in high temp high pressure environments

23
Q

Most folds are

A

result from compressional stresses that result in a shortening and thickening of the crust

24
Q

Anticlines

A

upfolded or arched sedimentary layers

Oldest strata in the center

25
Synclines
downfolded or troughs of rock | youngest strata are in the center
26
symmetrical
the limbs of the fold are mirror images of each other
27
asymmetrical
the limbs of the fold are not identical - Overturned : one or both limbs are titled beyond vertical - Plunging- the axis of the fold penetrates the ground
28
Domes
upwarped circular features
29
Basins
Downwarped circular features | looks like a bowl
30
Monoclines
large, steplike folds in the otherwise horizontal sedimentary strata Fold with one limb
31
Strike and Dip
sedimentary rocks that are inclined or bent indicate that the layers were deformed folowing deposition
32
Strike
Compass DIRECTION of the line produced by the intersection of an inclined rick layer or fault in a horizontal plate
33
Dip
ANGLE OF INCLINATION of the surface of a rock unit or fault measured from a horizontal plane
34
Faults
Fractures in rocks where displacement happened
35
slickenslide
polished smooth surfaces that happen from movement along a fault
36
Dip-Slip Fault
when movement is parallel to inclination Moves up and down along dip produces fault scarps
37
Normal Dip-Slip faults
hanging wall moving DOWN relative to the footwall {Tension} | Reverse fault moves up the footwall {Pressure}
38
horst
Uplifted blocks
39
grabens
Down-dropped blocks
40
Strike slip faults
moves horizontal and parallel to the strike - side by side
41
Oblique-slip faults
both a strike-slip and dip-slip movement