PLATE TECTONICS: The Grand Unifying Theory Of Geology Flashcards

1
Q

This is a hypothesis that suggested all present continents once existed as a sngle supercontinet known as ¨pangaea¨.

A

Continental Drift Theory

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2
Q

A german meteorologist and geophysicist who wrote ¨The Origin of Continents and Oceans¨.

A

Alfred Wegener

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3
Q

200 million years ago, the supercontinent began breaking into smaller continents, which then drifted to their positions.

A

Pangaea

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4
Q

What is the first evidence of the continental drift theory?

A

The continental jigsaw puzzle

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5
Q

Two other associates constructed a map that pieced together the edges of the continental shelves of South America and Africa at a depth of about 900 meters.

A

Sir. Edward Bullard

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6
Q

What is the second evidence of the continental drift theory?

A

Fossil Evidence

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7
Q

A freshwater reptile incapable of swimming the 5000 kilometers of open ocean that now separate the continents.

A

Mesosaurus

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8
Q

A fossil ¨seed fern¨identified by its tongue’shaped leaves and seeds, found in Australia, Africa, South America, Antartica, and India (it only grew on subpolar cliamtes)

A

Glossopteris

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9
Q

A land- dwelling reptile

A

Lystrosaurus

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10
Q

What is the third evidence of the continental drift theory?

A

Rock Types and Geologic Structures

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11
Q

Who found the 2.2- billion- years old igneous rocks in Brazil that closely resembled similarly aged rocks in Africa.

A

Alfred Wegener

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12
Q

What is the fourth evidence of the continental drift theory?

A

Ancient Climates

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13
Q

What climate was discovered in Southern Africa, South Aerica, Australia, and India?

A

Glacial Period that dated to the late Paleozoic

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14
Q

This is known to be the uppermost mantle and the overlaying crust behave sa a strong, rigid layer

A

Lithosphere

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15
Q

What do you call crust broken into segments?

A

Plates

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16
Q

The lithosphere overlies a weak region in the mantle known as the _______________.

A

Asthenosphere

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17
Q

What was the main objections towards the continental drift theory?

A

Its inability to provide an acceptable mechanism for the movement of the continents.

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18
Q

Any plate within an area greater than 20 million km^2

A

Major plate

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19
Q

How many major plates are there?

A

7 major plates

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20
Q

What is the largest major plate?

A

Pacific plate

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21
Q

Any plate with an area less than 20 million km^2

A

Minor plate

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22
Q

Any plate with an area less than 1 million km^2

A

Microplate

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23
Q

What are the three types of plate boundaries?

A
  • Divergent boundaries
  • convergent boundaries
  • transform boundaries
24
Q

Constructive margin

A

Divergent Boundary

25
Destructive Margin
Convergent boundary
26
Conservative margin
Transform fault boundaries
27
This is also called ¨spreading centers¨
Divergent boundary
28
Boundaries between two plates that are diverginf or MOVING AWAY from each other.
Divergent Boundary
29
Give two examples of divergent boundary
- mid- oceanic ridge | - continental rift zone
30
This is the longest topographic feature on the earth´s surface
Global ridge system (Mid- atlantic ridge, east pacific rise, and mid- indian ridge)
31
The boundaries between two plates that are converging or MOVING TOWARDS each other
Convergent boundary
32
What are the three types of convergent boundaries?
- oceanic- continental = volcanic arc - oceanic- oceanic = island arc - continental- continental = mountain range
33
An ocean floor plate collides with a less dense continental plate
Oceanic- continental = volcanic arc
34
An ocean floor plate collides with another ocean floor plate
Oceanic- oceanic = island arc
35
A continental plate collides with another continental plate
Continental-continental = mountain range
36
The boundaries between two paltes that are sliding horizontally past one another.
Transform Fault Boundaries
37
Two types of Tranform Fault Boundaries
1. Left-lateral strike-slip or sinistral fault | 2. Right-lateral strike-slip or dextral fault
38
Rift valleys in mid-oceanic ridges
Divergent in oceanic crust
39
Rift Valleys in continental rift zones
Divergent in continental crust
40
Mountain ranges
Convergent that is continental- continental
41
Volcanic arcs
Convergent that is oceanic- continental
42
Island arcs
Convergent that is oceanic- oceanic
43
Faults
Transform Fault
44
Denser Plate
Oceanic plate
45
What causes the movement of plate tectonics?
Mantle convection
46
What is the primary mechanism of transporting heat away from the Earth´s interior to the surface where it is eventually radiated into space.
Convective flow in the mantle
47
What are the two evidences of plate tectonics?
Ocean Drilling and Hot Spots
48
This hypothesis predicted that the youngest oceanic crust would be found at the ridge crest, the site of seafloor production, and the oldest oceanic crust would be located adjacent to continents.
Seafloor-spreading hypothesis by Harry Hess
49
This showed that the volcanoes increase in age with increasing distance from the ¨big island¨of Hawaii.
Radiometric dating of the Hawaiian Island- Emperor Seamount chain
50
Due to the pacific plate moving over the hot spot, a chain of volcanic structures known as ______________ was built.
Hot-spot track
51
What are the forces that drive plate motion
1. Ridge Push | 2. Slab pull
52
This gravity’driven mechanism results from the elevated position of the oceanic ridge,w here causes slabs of litosphere to ¨slide¨down the flanks of the ridge.
Ridge Push
53
During subduction as these cold, dense oceanic litosphere sinks into the asthenosphere, they ¨pull¨the trailing plate along.
Slab Pull
54
This layered model has two zones of convection— a thin, dynamic layer in the upper mantle and a thick, sluggish once a located below.
Model 1: Layering at 660 kilometers
55
This model sucessfully explains why basaltic lavas that erupt along the oceanic ridges have a different chemical make- up than those that erupt in Hawaii as a result of hot-spot activity.
Model 1: Layering at 660 kilometers
56
This model suggests that the burial ground of subducting slabs in the core-mantle boundary.
Model 2: Whole Mantle Convection
57
This material melts and buoyantly rises toward the surface as a mantle plume.
Model 2: Whole Mantle Convection