G10 Tectonic Plates Flashcards

(69 cards)

1
Q

Blocks that are primarily sturdy, with margins that trace earthquake zones lying along the network of ridges and trenches

A

Tectonic Plates

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2
Q

Models for Plate Movement

A

Kinematics and Dynamics

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3
Q

structures are examined and compared to the movements of blocks of Earth’s surface, ignoring underlying forces.

A

Kinematics

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4
Q

forces and processes resulting in material movement throughout Earth

A

Dynamics

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5
Q

is the continental drift hypothesis and seafloor spreading hypothesis combined.

A

Plate Tectonic Theory

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6
Q

Argues close kinship among sets of continents, as well as their geological characteristics.

A

Continental Drift Theory

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7
Q

The Earth’s ancient supercontinent

A

Pangaea

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8
Q

Explains the formation of new oceanic crust which leads to the movement of plates.

A

Seafloor Spreading

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9
Q

There are only seven major plates which include

A
North America, 
South America, 
Pacific, 
African, 
Eurasian, 
Australian-Indian, and 
Antarctic plates.
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10
Q

Factors Affecting Plate Movements

A

Solid-state flow model, Hotspots

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11
Q

Relies on temperature and phase changes.

A

Solid-state flow model

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12
Q

Areas with abnormally high volcanic activity hat have remained stationary for a very long time.

A

Hotspot

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13
Q

radioactivity causes magma to rise where it expands to produce the plates above Earth’s surface.

A

Solid-State Flow Model

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14
Q

The _, _ plates descend, replacing the hotter material below.

Can be likened to a kettle.
(Solid-State Flow Model)

A

older, denser

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15
Q

gravitational factors

A

ridge push, slab pull

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16
Q

This is a force that causes hotter, less dense material to force itself up through a ridge.

A

Ridge push

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17
Q

This is the pulling of oceanic lithosphere downward at subduction zones.

A

Slab pull

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18
Q

3 main processes that affect mantle convection

A

heating at the bottom caused by the heat loss from Earth’s core.

heating due to radioactive decay

cooling on the surface creating thick, cold lithospheric slabs denser than the mantle.

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19
Q

is the supercontinent of ancient Earth.

A

Pangaea

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20
Q

The northern landmass was

Pangaea

A

Laurasia

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21
Q

The southern landmass(Pangaea)

A

Gondwana

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22
Q

Evidence that Supports Plate Movement

A

Continental Fit, Fossil Evidence, Paleomagnetic Data,

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23
Q

Some continents’ shapes fit each other.

Scientists believe, with evidence, that these continents were once connected to each other.

A

Continental Fit

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24
Q

can be found in separate continents even though they are from the same species.

A

Fossils of animals and plants

Fossil evidence

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25
Specific deposits also provide _ _ _ in conditions across continents. (Fossil Evidence)
evidences of similarities
26
a series of rock deposits that provides evidence for these assemblages (Fossil Evidence)
Gondwana Rock Succession
27
has an influence of patterns in rocks, which coincide with shifts in the _ _ _ (Paleomagnetic Data)
Earth's magnetic pole
28
The Earth’s magnetic pole has an influence of patterns in rocks, which coincide with shifts in the Earth’s magnetic pole. This serves as evidence because their magnetic north was found to be _.
discordant
29
Can rock patterns be founf in Reykjanes Ridge?
Yes
30
implications of Plate Tectonics
``` rate of plate movements, geologic history of localities, mineral explorations, hazard predictions, and urban planning ```
31
Plate tectonics elucidates the geologic history of localities by providing an explanation for the regional settings and processes of an area, painting a more vivid picture of the geologic record. (Geologic History)
-
32
As a result of tracing an area’s geologic history, mineral explorers (Mineral Explorations)
can more easily trace and quantify deposits
33
Geologic maps show these features.
-
34
Most of the seismicity can be found | Hazard Prediction
along plate boundaries
35
Studying these boundaries can allow humans to | Hazard Prediction
predict any hazards within the area.
36
Only _ was connected to other landmasses in the past. The rest of the Philippines emerged from the ocean.
Palawan
37
Other crustal movements that are not related to seismic activities. These are usually less intense compared to seismic activity.
Aseismic Activity
38
As a result of hazard predictions, humans can also properly plan the arrangement of urban settlements.
Urban Planning
39
Institutes in the Philippines that study seismology
DOST, PHIVOLCS
40
DOST
The Department of Science and Technology
41
PHIVOLCS
The Philippine Institute of Volcanology and Seismology, an arm of DOST.
42
Fossil assemblages among the continents possess differences, indicating that the fossilized organisms had to have crossed the continents via _ _.
land bridges
43
is a specific temperature at which materials change or lose their magnetism
Curie point
44
is not static, rather, it frequently switches polarities. These changes are referred to as magnetic reversals.
Earth’s magnetic field
45
Earth’s magnetic field frequently switches polarities. These changes are referred to as
magnetic reversals
46
Plates move extremely slowly most of the time for extended periods of time. This slow movement is referred to as
creep
47
Crustal movements having less intensity than those related to tectonic belts are classified as
aseismic
48
is in charge of reducing the impacts of natural disasters.
Philippine Institute of Volcanology and Seismology (PHIVOLCS)
49
developed, was widely advocated by ​ Alfred Wegener in 1915.
Continental Drift Theory
50
developed, was widely advocated by ​ Alfred Wegener in 1915.
Continental Drift Theory
51
In 1962, Harry Hess pioneered the concept of
seafloor spreading
52
a specific point where three plate boundaries converge
triple junction
53
arm of the triple junction that failed to | produce an ocean basin, it is referred to as an
aulacogen
54
In the 1930s, ​ Arthur Holmes heavily advocated
solid-state flow model
55
moves material underneath the plates | sideward, but its effect is​ so small that it is considered negligible
Mantle drag
56
are rising columns of hot rocks from the lower mantle and cause melting ​ as they reach the surface, hence another mechanism for plate motion
Mantle plumes
57
mantle is divided into two zones of convection which is a thin layer in the upper mantle at a depth of 660 kilometers and a thick layer located below. This model is known as ​
layer cake model
58
where denser oceanic lithosphere sinks and may even reach the core-mantle boundary. This material eventually melts and rises toward the surface of Earth.
whole mantle convection
59
indicate a large ice sheet encompassing broad areas of | today’s southern continents
Glacial deposits
60
marked an | ancient desert
evaporites and sandstones
61
rates of continental advancement and seafloor spreading are determined by measuring the _ _ _ _ _ _ _ _. In fact, the locations of the continents prior to Pangaea’s breakup were also accurately pinpointed through this method
widths of the magnetic stripes on the seafloor
61
rates of continental advancement and seafloor spreading are determined by measuring the
widths of the magnetic stripes on the seafloor
62
oceanic plate's speed
6-9cm
63
oceanic plate's speed
6-9cm/year
64
continental plate's speed
2 cm/year
65
elucidates the geologic history of localities by providing an explanation for the regional settings and processes of an area, painting a more vivid picture of the geologic record
Plate tectonics
66
an essential material in mineral explorations. It provides various information that is important in locating for new mineral deposits. It makes use of the morphology of rocks bodies as well as age relationships between rock units.
geologic map
67
``` use surface modifications that are being recorded with time which can be used to make three or four-dimensional geologic models. ```
Tectonic processes
68
areas where | settlements must not be built
​ permanent danger zones