Geology 101 Quiz 2 Flashcards

1
Q

if any plate moves, it must immediately (3 things)

A
  1. run into another plate in the direction it is moving
  2. pull away from a plate on the opposite side
  3. grind laterally past plates on the sides
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2
Q

three types of tectonic boundaries or zones

A

divergent, convergent, transform fault

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3
Q

divergent boundaries

A

where two plates pull apart

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4
Q

convergent boundaries

A

where two plates collide

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5
Q

transform fault boundaries

A

where to plates slide past one another

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6
Q

divergent boundaries will occur

A

above rising convection cells

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7
Q

convergent boundaries will occur

A

where convection cells are falling downward

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8
Q

when plates pull apart (divergence), what happens?

A

magma from the mantle fills the gap and creates new oceanic crust

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9
Q

when plates collide (convergence), what happens?

A

plates will either crumple, or one plate will slide beneath the other, a process known as subduction

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10
Q

plates sliding past one another (transform faults) form ?

A

fault zones

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11
Q

the appearance of the surface of the earth is controlled in large part by

A

the type of tectonic boundaries present, and whether the plate boundary is oceanic or continental

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12
Q

examples of oceanic-oceanic plate divergent boundaries

A

mid-atlantic ridge, east pacific rise

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13
Q

oceanic-oceanic plate divergent boundaries feature

A

elevated ridge on ocean floor, earthquake activity common, sea floor lava flows, thermal vents (super heated water)

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14
Q

the mid-atlantic ridge falls exactly in the middle of

A

the Atlantic between North/South America and Europe/Africa

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15
Q

the mid-atlantic ridge divergent zone passes through Iceland, which is a good example of

A

divergence in continental crust

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16
Q

continental-continental plate divergent boundaries examples

A

Iceland, Great Rift Valley (Africa)

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17
Q

continental-continental plate divergent boundaries feature

A

elevated ridge with rifted valley; earthquake activity common; lava flows; narrow, inland seas

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18
Q

Iceland periodically loses a town to

A

lava flows emanating from rifts

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19
Q

Great Rift Valley (East African Rift) is actually a

A

three pointed star-shaped rift

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20
Q

the ? and the ? are rifts filled in with water (narrow inland seas)

A

Red Sea, Gulf of Aden

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21
Q

continental-oceanic plate divergent boundaries are not seen because

A

oceanic crust is generated on either side of the rift, so it readily turns into an oceanic-oceanic plate boundary

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22
Q

continental-oceanic plate convergent boundaries examples

A

Pacific Northwest (Mt. St. Helens area), Andes Mountains/Peru-Chile Trench

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23
Q

continental-oceanic plate convergent boundaries feature

A

volcanic mountains on continental parallel to coast, subduction of oceanic plate - creates ocean trench parallel to coast, deep earthquakes from subducting plate

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24
Q

when oceanic crust meets continental crust, which always loses and why?

A

oceanic crust (it’s thinner and sits lower)

25
friction from ? plates generates tremendous heat; overlying rock material melts and moves upward and ?
subducting; erupts as volcanoes
26
when subduction begins, the downward bend results in
a deep trench
27
the trenches from subduction form the
deepest places on earth (some are under nearly 7 miles of water, which is much deeper than Mount Everest is tall)
28
volcanic mountains typically form directly above
the subducting plate
29
Mt. St. Helens and Mt. Rainier are active volcanoes because of
subduction of the Juan de Fuca Plate
30
oceanic-oceanic plate convergent boundaries examples
Japan, Aleutian Islands, Philippines
31
oceanic-oceanic plate convergent boundaries feature
volcanic island arc, ocean trench parallel to island arc, deep earthquakes from subducting plate
32
subduction of one plate produces
volcanism and island building
33
the perimeter of the Pacific is known as the "Ring of Fire" because
its lined with earthquake epicenters and volcanoes
34
continental-continental plate convergent boundaries examples
Himalaya Mountains
35
continental-continental plate convergent boundaries feature
non-volcanic mountains (inland), lots of earthquakes
36
the ? are the tallest mountains in the world because of ?
Himalayas; active collision and buckling of two colliding continental plates
37
continental-continental plate transform fault boundaries examples
San Andres Fault, California
38
continental-continental plate transform fault boundaries feature
strike-slip faults, shallow earthquake activity
39
strike-slip faults
faults with no vertical displacement (both sides move horizontally)
40
oceanic-oceanic plate transform fault boundaries examples
Mid-Atlantic Ridge, East Pacific Rise
41
oceanic-oceanic plate transform fault boundaries feature
strike-slip faults, shallow earthquake activity
42
continental-oceanic plate transform fault boundaries
not seen b/c oceanic crust sits lower and is thinner; since lateral movement is never perfectly parallel, the weaker oceanic plate quickly starts to subduct; it thus becomes a convergent zone
43
Hot Spots
relatively stationary areas of the mantle that are particularly hot, which periodically melt through the overlying crust to produce a volcano
44
Hot Spots examples
Hawaii; Yellowstone National Park, Wyoming
45
Hot Spots feature
mid-plate volcanism
46
because the overlying plate is moving, the periodic volcanism of hot spots results in
a string of volcanoes that get older the farther they are from the current volcanic activity
47
number of plates (are/are not) fixed
are not
48
oceanic plates (can/cannot) disappear
can (if two continents approach each other and collide, the ocean that was between them will completely subduct and disappear)
49
continents (do/do not disappear), they (are/are not) buoyant
do not; are (when continents collide, they become a single land mass)
50
new plates can form by
breaking existing plates
51
continents (can/cannot) grow
can (islands that form and later collide with a continent add additional land to the continent; the islands will not subduct)
52
What evidence did Alfred Wegener see that continents have drifted over time?
1. "Jig saw puzzle" fit of continents 2. rock types and fossil types on different continents matched 3. the presence of glacial deposits and glacial scrape marks on all the continents that all grouped together if the continents were put together
53
none of Wegener's observations were convincing enough until ?
reversals were discovered in seafloor magnetism
54
when iron-bearing magma solidifies (hardens into rock), the iron minerals ...
align along the earth's magnetic field
55
the earth's magnetic field (has/has never) reversed
has (and many times)
56
we can tell the earth's magnetic field has reversed because
successive lava flows on the same volcano will have iron minerals oriented in one direction in one flow, and reversed in the opposite direction in a later flow
57
bands run (parallel/perpendicular) to mid-ocean ridges with reversing magnetic orientation
parallel
58
stations set up around the world have documented that the distance between Europe and North America
increases by several centimeters each year