G10 Plate Boundaries Flashcards

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1
Q

states that the lithosphere is a strong rigid layer the uppermost mantle and crust that were broken into several major and minor segments called tectonic plates.

A

Plate Tectonics Theory

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2
Q

Major Plates

A
North America
South America
Pacific
African
Eurasian
Australian-Indian
Antarctic plates.
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3
Q

three main types of plate boundaries

A

divergent
convergent
transform

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4
Q

is formed when two plates move away from each other resulting to upward movement of molten material and formation of new seafloor

A

divergent boundary

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5
Q

landform produced by a divergent boundary

A

ocean floor

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6
Q

is formed when two plates move toward each other

A

convergent boundary

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7
Q

convergent boundary is also known

A

destructive margin

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8
Q

is where the oceanic crust is destroyed and recycled.

A

convergent boundary

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9
Q

types of convergent boundaries

A

oceanic-oceanic

continental-continental

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10
Q

When two oceanic crusts converge, the _ oceanic block sinks beneath the other.

A

denser

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11
Q

oceanic-oceanic convergence produces a

A

volcanic island arc or island arc

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12
Q

When two continental plates converge, it produces spectacular mountain ranges, also known as _, such as the Himalayas.

A

orogens

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13
Q

occurs when two plates simply slide past each other

A

transform fault boundary

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14
Q

In this type of boundary, there is no formation or destruction of the new lithosphere.

A

transform fault boundary

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15
Q

a zone in the Earth’s crust where the plates move away from each other

A

Divergent boundaries

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16
Q

also known as the spreading centers.

A

Divergent boundaries

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17
Q

is where the continents split apart and form new continental margins

A

Divergent boundaries

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18
Q

Divergent plate boundaries are considered as _ _ because it’s where the new ocean floor is generated.

A

constructive margins

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19
Q

Elevated areas in the seafloor forms mountain system called the _ _.

A

mid-ocean ridge

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20
Q

These underwater mountains are linked in chains with valleys known as _.

A

rift

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21
Q

is the main mechanism operating along divergent margins.

A

Seafloor spreading

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22
Q

continuous process occurring in mid-oceanic ridges in which both sides of the ridge move apart, causing the spreading.

A

Seafloor spreading

23
Q

As new seafloor moves away from both sides of the ridge, more melts arise from the asthenosphere. This process is repeated in a _ _- like manner.

A

conveyer belt

24
Q

Spreading of landmasses into two segments forms

A

continental rifts

25
Q

areas where tectonic plates move

towards each other

A

Convergent plate boundaries

26
Q

are often associated with subduction zones, where oceanic crust descends towards the mantle due to differences in density of the subducting plate, the asthenosphere, and the overriding plate

A

Convergent plate boundaries

27
Q

oceanic crust descends towards the mantle due to differences in _ of the subducting plate, the asthenosphere, and the overriding plate

A

density

28
Q

oceanic lithosphere is destroyed along trenches and is recycled back into the asthenosphere

A

Subduction

29
Q

are long, sublinear chains of volcanoes following the orientation of ocean trenches

A

Arcs

30
Q

the denser oceanic crust subducts under the lighter continental crus

A

oceanic-continental convergent margins

31
Q

oceanic-continental convergent margins form

A

volcanic arcs

32
Q

the older and much denser plate subducts under the younger plate

A

oceanic-oceanic convergent margins

33
Q

oceanic-oceanic convergent margins form

A

volcanic island arcs

34
Q

Convergent plate boundaries may also develop through the collision of two continental plates, by

A

continental-continental convergent margin

35
Q

forms mountain ranges with linear elevated regions.

A

continental-continental convergent margin

36
Q

a continuous process occurring in mid-oceanic ridges in which both sides of the ridge move apart.

A

seafloor spreading

37
Q

.

Movement in the boundaries induces decompression melting of rocks and form new oceanic lithosphere.

A

-

38
Q

The primary process operating in oceanic convergent margins is _

A

subduction

39
Q

are long, sublinear chains of volcanoes following the orientation of ocean trenches.

A

arcs

40
Q

(Divergent boundaries)occurs within a continent and is caused by opposing tensional forces that stretch and thin the lithosphere, causing the outermost crustal rocks to break through normal faulting, thus forming a continental rift

A

Continental rifting

41
Q

(Divergent boundaries)may form between two rifted continents once the lithosphere thins sufficiently for magma to erupt along an axis

A

New ocean basins

42
Q

form different landforms and involve different processes depending on the type of plates involved in the collision

A

Convergent plate boundaries

43
Q

the denser oceanic crust subducts under the lighter continental crust. This process forms continental volcanic arcs.

A

oceanic-continental convergent margins

44
Q

the older and much denser plate subducts under the younger plate. This process forms volcanic island arcs.

A

oceanic-oceanic convergent margins

45
Q

Convergent plate boundaries may also develop through the collision of two continental plates, by

A

continental-continental convergent margin.

46
Q

forms mountain ranges with linear elevated regions.

A

continental-continental convergent margin

47
Q

are characterized by horizontal motion along transform fault systems parallel to the boundary separating two plates form fault systems around the world

A

Transform plate boundaries

48
Q

are part of curvilinear breaks in the seafloor known as _

A

fracture zones

49
Q

home to landforms including continental rifts and oceanic ridges.

A

Divergent plate boundaries

50
Q

gives rise to landforms known as continental volcanic arcs

A

Convergence

51
Q

forms volcanic island arcs, or simply, island arcs.

A

oceanic-oceanic convergence,

52
Q

involves a buoyant landmass (continents, arcs) moving towards the margin of another buoyant landmass due to the subduction of an intervening seafloor forming orogenic plate.

A

Continental-continental (C-C) convergence

53
Q

are part of curvilinear breaks in the seafloor known as fracture zones.

A

Transform faults