Plate Tectonics Flashcards

(35 cards)

1
Q

its lightest, most buoyant rock layer?

A

Crust

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2
Q

The mostly-solid bulk of Earth’s interior. It lies between Earth’s dense, super-heated core and its thin outer layer, the crust

A

Mantle

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3
Q

from Ancient Greek “asthenós” meaning ‘without strength’ is the mechanically weak and ductile region of the upper mantle of Earth.

A

Asthenosphere

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4
Q

Is the third layer of the Earth. It is the only liquid layer and is mainly made up of the metals iron and nickel. Responsible for Earth’s magnetic field

A

Outer Core

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5
Q

Is a hot, dense ball of (mostly) iron.

A

Inner Core

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6
Q

Derived from a Greek word “tekton” which means “carpenter” or “builder”.

A

Tectonic

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7
Q

A plate is a large, rigid slab of solid rock that is formed from the lithosphere.
The plates “float” on the slowly flowing asthenosphere.
The plates include both the land and ocean floor.

A

Tectonic Plates

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8
Q

It is where Earth is likened to a grape that contracted due to a cooling process that occurred after the Big Bang about 13.77 billion years ago.

A

Raisin Theory

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9
Q

In 1889, American Seismologist and Geologist, Charles Edward Dutton, proposed the term

A

Isostasy

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10
Q

Isostasy states that whenever equilibrium exists in the Earth’s surface,

A

equal mass must underlie equal surface areas

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11
Q

It states that the Earth’s outer most layer is fragmented into dozen, or more large and small solid plates called Lithospheric plates or Tectonic plates, that glide over Earth’s mantle, the rocky inner layer above Earth’s core.

A

Continental Drift Theory

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12
Q

What is the first world atlas, which is developed and published by Abraham Ortelius on January 1, 1596

A

Theatrum Orbis Terratrum

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13
Q

Alfred Wegener, German Climatologist proposed the , in his book
The Origin of the of the Continents and Ocean in 1915.

A

Continental Drift Theory

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14
Q

What is the name of the supercontinent?

A

PANGAEA

“All Earth”

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15
Q

Wegener also explained that 1,100 million years ago, there was another super continent that predated the Pangaea, named Rodinia, which is Russian for

A

“motherland, birthplace”

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16
Q

During the late Triassic period, Pangea began to break up into two smaller supercontinents called, which move to the northern
and southern extremes of the planet, respectively.

A

Laurasia and Gondwanaland

17
Q

What surrounds the Pangaea, It was formed approximately

356 mya, while the two continents were separated by Tethys Sea 251 to 65.5 mya.

A

Panthalassa vast ocean

18
Q

Number of Crustal Plates

A

58 Crustal Plates, 15 Major Tectonic Plates, 7 or 8 Primary Plates and the remaining are Smaller Plates

19
Q

It is the outermost layer of Earth’s lithosphere
that makes up the planet’s continents and
continental shelves. It is composed of lower-density
materials such as granitic rocks.

A

Continental Lithosphere

20
Q

Is made up of heavier basalt and

gabbro rocks. It is formed by magma

A

Oceanic Lithosphere

21
Q

describes the movement of
the mantle as it transfers heat from the white-hot
core to the brittle lithosphere.

A

Mantle Convection Theory

22
Q

occurs because relatively hot rocks are less dense and rise in a gravitational field while relatively cold rocks are denser and sink.

A

Mantle Convection Theory

23
Q

This theory states that gravity and the plates
themselves are the ones responsible for the plate
tectonics through subduction process.

A

Slab Pull Theory

24
Q

One type of evidence that strongly
supported the Theory of Continental Drift is
the fossil record. Fossils of similar types of
plants and animals in rocks of a similar age
have been found on the shores of different
continents, suggesting that the continents
were once joined.

A

Paleontological Evidence

25
The hypothesis that the continents were once connected also helps to better explain the glacial striations and tills found in South America, Africa, India, and Australia. This body of evidence suggests that these areas were once connected and covered by glacial ice, which flowed outwards from Antarctica.
Evidence from Glaciation
26
Along with the development of reliable world maps in the early 20th century, geographers' notices that the coastlines of several of the present-day continents would perfectly fit together.
Evidence from Structure and Rock | Type
27
the study of the extended climatic conditions of the past | geologic era.
Paleoclimatology
28
The magnetic minerals in the rock layers prove that the Magnetic poles have reversed multiple times over geologic period at the mid-ocean ridges. Once heated materials are produces are the ridges, magnetic materials align themselves with the Earth’s magnetic field. When rocks cool down, the minerals are preserved in their aligned state. Samples collected from both sides of ridges show parallel strips of normal and reversed polarities
Evidence from Paleoclimate
29
The study of the ancient magnetic fields. Using a sensitive instrument called a magnetometer.
Paleomagnetism
30
These are areas where two or more tectonic | plates bump into each other, also known as
Collision Zone
31
Areas where two or more tectonic plates are | moving away from each other also called as
Extensional boundary
32
Also known as a destructive plate boundary. It occurs when two plates are pushing towards each other. Here, the crust is destroyed and recycled back into the interior od the Earth, while one plate dives under another.
Convergent Boundary
33
Also known as a constructive boundary, this plate the boundary is characterized by tensional stresses that normally produce long rift zones, normal faults and basaltic volcanism.
Divergent Boundary
34
the regions where a portion of the tectonic plates are diving beneath other plates into the Earth’s interior.
Subduction zones
35
neither creates nor destroys a crust,
Transform Boundary