Chapter 7: Plate Tectonics: A Science Revolution Unfolds Flashcards

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1
Q

Continental Drift

A

the hypothesis that continents are mobile and are not fixed in place
(Proposed by Alfred Wegener)

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2
Q

German meteorologist
Published “Origins of Oceans and Continents” -1915
Hypothesized a former super continent, Pangaea

A

Alfred Wegener

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3
Q

“Continental Drift” Hypothesis

A
  1. The idea that a supercontinent, Pangaea began breaking apart 200 million yrs ago.
  2. Continents were thought to have “drifted” to present positions
  3. Idea was that continents “broke” though the ocean crust
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4
Q

An ancient ocean that existed before the moving of the continents was called what?

A

Panthalassa

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5
Q

Pieces of evidence that show the continents were once a whole mass?

A
  1. All continents fit together
  2. Fossils match up across continents
  3. Mountain ranges match up
  4. Locations of past glaciations
  5. Paleoclimatic evidence
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6
Q

What allows the crust to be recycled?

A

Subduction

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7
Q

Pieces of Earth’s surface moves in what ways?

A

a) Grind sideways (transform faults)
b) Collide together (continent-continent collisions)
c) Sink into Earth;s hot interior (subduction)

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8
Q

One of the driest places in the world is?

A

Atacama Dessert

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9
Q

The rigid outer rind of the Earth, which makes up the tectonic plates.

A

The Lithosphere

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10
Q

the inner, more easily deformed layer that acts more like a plastic.

A

The Asthenosphere

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11
Q

The Lithosphere is broken into about how many plates?

A

12 large plates and 8 smaller plates.

combos of continental and oceanic areas

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12
Q

The Continental Crust

A

a) Silica-rich
b) LOW density of 2.7 g/cm
c) Stands HIGHER than denser oceanic crust

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13
Q

The Oceanic Crust

A

a) Iron & magnesium- rich and poor-silica
b) HIGHER density of 3.0 g/cm
c) 7 km thick
d) Floats LOWER than continental crust, on top of denser mantle

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14
Q

A boundary between that crust and mantle was identified by a density difference called what?

A

The Mohorovicic Discontinuity (“The Moho”)

marks the boundary base of the Earth’s crust

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15
Q

The three types of plate motions?

A
  1. Divergent Boundaries
  2. Convergent Boundaries
  3. Transform Boundaries
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16
Q

What is a Divergent Boundary?

A

Plates move away from each other, usually at mid-oceanic ridges.
AKA it creates a new seafloor.

EX: East African Rift
<== | ==>

17
Q

What is a Convergent Boundary?

A
Plates move towards each other.
O    -    C = Continental Volcanic Arc (Mt. St. Helens)
^down ^ over 
O-O = Island Volcanic Arc (Aleutians)
C-C =  Creation of Mountains (Himalayas)
==> |<==
18
Q

What is a Transform Boundary?

A

Plates slide/grind past one another.

Transforms Faults (San Andreas Fault)

Associated w/ earthquakes NOT volcanoes.
^ | > (down)

19
Q

What evidence is there from drilling the ocean floor?

A

A) The ocean floor is youngest in the center, older away from spreading center.
B) Thickness of ocean-floor sediments verifies seafloor spreading.

20
Q

What is the STRONGEST evidence of the seafloor spreading?

A

Paleomagnetism

21
Q

Ancient magnetism is preserved in rocks as they form, is called what?

A

Paleomagnetism

22
Q

What is a Hot Spot?

A

A) Caused by rising plumes of mantle material

B) Volcanoes can form over hot spots, eventually forming islands out in the ocean

23
Q

What are Mantle Plumes?

A

A) Long-lived igneous structure

B) Some originate at great depth, perhaps at the mantle-core boundary.

24
Q

Give an example to a Hot Spot

A

The Hawaiian Islands

25
Q

How can we measure tectonic plate motion?

A

1) By using hot spot “tracks”
2) Using space-age technology to directly measure the relative motion of plates. (GPS)
(Islands furthest away from a hot spot are the oldest)

26
Q

What drives tectonic plate motion?

A

A) Earth’s heat is the driving force
B) Slab-pull
C) Ridge-push

27
Q

Slab-Pull and Ridge-Push Model

A
  1. Descending oceanic crust pulls plate down
  2. The elevated mid-ocean ridge system pushes plate apart and away (gravity)

EX: sheets falling off the bed

28
Q

Plate-Mantle Convection Model

A

Mantle plumes extend from mantle-core boundary and cause convection within the mantle (how a lava lamp functions)

29
Q

Two main sub-models that are proposed for the plate-mantle convection?

A

A) layering at 660 kilometers
OR
B) Whole-mantle
convection