plate tectonics (2) Flashcards

1
Q

Plate Tectonics

A

A theory which proposes that Earth’s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and the crust itself

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2
Q

Describe the view held by most geologists prior to the 1960s regarding the ocean basins and continents.

A

They believed that the continents didn’t move

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3
Q

Name the 20th century hypothesis that was at first rejected and then the theory that later replaced it.

A

Continental Drift Hypothesis

The Theory of Plate Tectonics

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4
Q

Continental Drift Hypothesis

A

A hypothesis, credited largely to Alfred Wegener, which suggests that all present continents once existed as a single supercontinent. Further, beginning about 200 million years ago, the supercontinent began breaking into smaller continents, which then “drifted” to their present positions

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5
Q

Supercontinent

A

A large landmass that contains all, or nearly all, of the existing continents

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6
Q

Pangaea

A

The proposed supercontinent that 200 million years ago began to break apart and form the present landmasses

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7
Q

What was the first line of evidence that led earthly investigators to suspect that the continents were once connected?

A

Shape

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8
Q

Explain why the discovery of the fossil remains of Mesosaurus in both South America and Africa, but nowhere else, supports the continental drift hypothesis.

A

Its a freshwater reptile, it lived in lakes not in oceans

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9
Q

In the early 20th century view of how land animals apparently migrated across vast expanses of open ocean?

A

They walked across skinny land bridges or floated on rafts

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10
Q

Describe two aspects of Wegener’s continental drift hypothesis that were objectionable to most Earth scientists

A

Mechanism of continental drift

Continents were moving independent of oceanic crust

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11
Q

Theory of Plate Tectonics

A

A theory which proposes that Earth’s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and the crust itself

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12
Q

Lithosphere

A

The rigid outer layer of Earth, including the crust and upper mantle

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13
Q

Asthenosphere

A

A subdivision of the mantle situated below the lithosphere. This zone of weak material exists below a depth of about 100 km and in some regions extends as deep as 700 km. The rock within this zone is easily deformed

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14
Q

Lithospheric Plate

A

A coherent unit of Earth’s rigid outer layer that includes the crust and upper unit

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15
Q

Divergent Plate Boundaries

A

Where two plates move apart

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16
Q

Convergent Plate Boundaries

A

Where two plates move toward each other

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17
Q

Transform Plate Boundaries

A

Where two plates grind past each other

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18
Q

What new findings about the ocean floor did oceanographers discover after World War II?

A

The seafloor is quite young, the sediment that was deposited was relatively thin-> seafloor is being recycle

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19
Q

Divergent Plate Boundary

A

A boundary in which two plates move apart, resulting in upwelling of material from the mantle to create new seafloor

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20
Q

Ocean Ridge System

A

A continuous elevated zone on the floor of all the major ocean basins and varying in width from 500 to 5000 km. The rifts at the crests of ridges represent divergent plate boundaries.

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21
Q

Rift Valley

A

A long, narrow trough bounded by normal faults, It represents a region where divergence is taking place.

22
Q

Seafloor Spreading

A

A hypothesis, first proposed in the 1960s by Harry Hess, which suggests that new oceanic crust is produced at the crests of mid-ocean ridges, which are the sites of divergence

23
Q

Continental Rift

A

A linear zone along which continental lithosphere stretches and pulls apart. Its creation may mark the beginning of a new ocean basin

24
Q

What is the average rate of seafloor spreading in modern oceans?

A

2 cm/yr in Atlantic
15 cm/yr in Pacific
Average: 5 cm/yr

25
Q

List four features that characterize the oceanic ridge system.

A

Long, elevated, linear, magma rising

26
Q

Convergent Plate Boundary

A

A boundary in which two plates move together, resulting in oceanic lithosphere being thrust beneath an overriding plate, eventually to be reabsorbed into the mantle. It can also involve the collision of two continental plates to create a mountain system

27
Q

Subduction Zone

A

A long, narrow zone where one lithospheric plate descends beneath another

28
Q

Deep-ocean Trench

A

A narrow, elongated depression of the seafloor

29
Q

Partial Melting

A

The process by which most igneous rocks melt. Since individual minerals have different melting points, most igneous rocks melt over a temperature range of a few hundred degrees. If the liquid is squeezed out after some melting has occurred, a melt with a higher silica content results

30
Q

Continental Volcanic Arc

A

Mountains formed in part by igneous activity associated with the subduction of oceanic lithosphere beneath a continent. Examples include the Andes and the Cascades.

31
Q

Volcanic Island Arc

A

A chain of volcanic islands generally located a few hundred kilometers from a trench where there is active subduction of one oceanic plate beneath another.

32
Q

Why does oceanic lithosphere subduct, while continental lithosphere does not?

A

Density, age determines temperature

old is cold and dense-> subducts

33
Q

What characteristic of a slab of oceanic lithosphere explains the formation of a deep oceanic trench as opposed to one that is less deep?

A

Density
The warmer it is the more buoyant it is
Deep trenches with deep subduction

34
Q

Transform Plate Boundary

A

A boundary in which two plates slide past one another without creating or destroying lithosphere

35
Q

Fracture Zones

A

A linear of irregular topography on the deep-ocean floor that follows transform faults and their inactive extensions

36
Q

Mantle Plume

A

A mass of hotter-than-typical mantle material that ascends toward the surface, where it may lead to igneous activity. These plumes of solid yet mobile material may originate as deep as the core-mantle boundary

37
Q

Hot Spot

A

A concentration of heat in the mantle, capable of producing magma that, in turn, extrudes onto Earth’s surface. The intraplate volcanism that produced the Hawaiian Islands is one example.

38
Q

Hot-Spot Track

A

A chain of volcanic structures produced as a lithospheric plates moves over a mantle plume

39
Q

Curie Point

A

The temperature above which a material loses its magnetization

40
Q

Paleomagnetism

A

The natural remnant magnetism in rock bodies. The permanent magnetization acquired by rock that can be used to determine the location of the magnetic poles and the latitude of the rock at the time it became magnetized

41
Q

Magnetic Reversal

A

A change in Earth’s magnetic field from normal to reverse or vice versa

42
Q

Normal Polarity

A

A magnetic field the same as that which presently exists

43
Q

Reverse Polarity

A

A magnetic field opposite that which presently exists

44
Q

Magnetic Time Scale

A

A scale that shows the ages of magnetic reversals and is based on the polarity of lava flows of various ages

45
Q

Magnetometer

A

A sensitive instrument used to measure the intensity of Earth’s magnetic field at various points

46
Q

What does the orientation of transform faults indicate about plate motion?

A

Parallel

47
Q

Which three plates appear to exhibit the highest rates of motion?

A

Pacific
Australia-India
Nazca

48
Q

Convection

A

The transfer of heat by the mass movement or circulation of a substances

49
Q

Slab Pull

A

A mechanism that contributes to plate motion in which cool, dense oceanic crust sinks into the mantle and “pulls” the trailing lithosphere along

50
Q

Ridge Push

A

A mechanism that may contribute to plate motion. It involves the oceanic lithosphere sliding down the oceanic ridge under the pull of gravity

51
Q

Which of these forces-slab pull or ridge push-contributes more to plate motion?

A

Slab pull (subduction zones)

52
Q

Describe the whole-mantle convection (plume) model.

A

Plumes rise from the core-mantle boundary

Subducted plates end up at the bottom of the mantle