Chapter 11, test 2: crustal deformation adn mountain building Flashcards

(32 cards)

1
Q

deformation

A

a general term that refers to all changes in the original form and/or size of a rock body.

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2
Q

stress

A

the forces that deform rock

compressional stress, and tensional stress

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3
Q

compressional stress

A

stress that squeezes and shortens rock mass

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4
Q

tensional stress

A

stress that pulls apart or elongates a rock mass

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5
Q

elastic deformation

A

like a rubber band the rock will return to nearly its original size and shape when stress is removed

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6
Q

brittle deformation

A

when the limit of rock strength is surpassed the rock fractures
low temp

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7
Q

ductile deformation

A

solid state flow (like water or taffy) that produces a change in shape without fracturing.
high temp

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8
Q

factors that influence the strength of a rock

A

temperature
confining pressure
rock type
time

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9
Q

temperature

A

high temp causes ductile deformation

low temp causes brittle deformation

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10
Q

confining pressure

A

greater pressure causes ductile deformation

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11
Q

rock type

A

sedimentary rocks and foliated metamorphic rocks deform by ductile deformation.
igneous tend to deform by brittle deformation

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12
Q

time

A

when techtonic forces are applied slowly over a long time, rocks display ductile deformation

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13
Q

folds

A

rocks bent in a series of waves
most folds result form compressional forces that shorten and thicken crust
types: anticline, syncline

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14
Q

anticline

A

up folded or arched rock layers

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15
Q

syncline

A

down folded rock layers

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16
Q

symmetrical

A

limbs mirror images

17
Q

asymmetrical

A

limbs are not mirror images

18
Q

overturned

A

one limb is tilted beyond the vertical

19
Q

faults

A

fractures or breaks in rocks along which appreciable displacement has taken place

20
Q

dip slip fault

A

movement along the inclination (dip) of fault plane

2 types: normal and reverse/thrust

21
Q

hanging wall

A

the rock above the fault surface

22
Q

footwall

A

the rock below the fault surface

23
Q

normal dip slip fault

A

hanging wall moves down
associated with fault block mountains
caused by tensional forces <>

24
Q

reverse dip slip fault

A

hanging wall moves up
caused by compressional stress ><
dips greater than 45 degrees

25
thrust dip slip fault
hanging wall moves up caused by compressional stress >< dips less than 45 degrees
26
megathrust earthquakes
due to shallow dip of the plate boundary large sections tend to get stuck these are most powerful earthquakes, a lot of tension builds up
27
strike slip fault
slide past each other dominant displacement in horizon often associated with plate boundaries
28
joints
fractures along with no appreciable displacement has occurred (no movement) example is arches national park
29
orogenesis
refers to processes that collectively produce mountain belts | example: laramide orogeny produced the rocky mountains
30
continental volcanic arc
oceanic-continental crust convergence
31
volcanic island arcs
oceanic-oceanic crust convergence
32
continental collisions
continental-continental crust convergence