G10 Plate Boundaries Flashcards

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
areas where tectonic plates move | towards each other
Convergent plate boundaries
26
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
Convergent plate boundaries
27
oceanic crust descends towards the mantle due to differences in _ of the subducting plate, the asthenosphere, and the overriding plate
density
28
oceanic lithosphere is destroyed along trenches and is recycled back into the asthenosphere
Subduction
29
are long, sublinear chains of volcanoes following the orientation of ocean trenches
Arcs
30
the denser oceanic crust subducts under the lighter continental crus
oceanic-continental convergent margins
31
oceanic-continental convergent margins form
volcanic arcs
32
the older and much denser plate subducts under the younger plate
oceanic-oceanic convergent margins
33
oceanic-oceanic convergent margins form
volcanic island arcs
34
Convergent plate boundaries may also develop through the collision of two continental plates, by
continental-continental convergent margin
35
forms mountain ranges with linear elevated regions.
continental-continental convergent margin
36
a continuous process occurring in mid-oceanic ridges in which both sides of the ridge move apart.
seafloor spreading
37
. | Movement in the boundaries induces decompression melting of rocks and form new oceanic lithosphere.
-
38
The primary process operating in oceanic convergent margins is _
subduction
39
are long, sublinear chains of volcanoes following the orientation of ocean trenches.
arcs
40
(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
Continental rifting
41
(Divergent boundaries)may form between two rifted continents once the lithosphere thins sufficiently for magma to erupt along an axis
New ocean basins
42
form different landforms and involve different processes depending on the type of plates involved in the collision
Convergent plate boundaries
43
the denser oceanic crust subducts under the lighter continental crust. This process forms continental volcanic arcs.
oceanic-continental convergent margins
44
the older and much denser plate subducts under the younger plate. This process forms volcanic island arcs.
oceanic-oceanic convergent margins
45
Convergent plate boundaries may also develop through the collision of two continental plates, by
continental-continental convergent margin.
46
forms mountain ranges with linear elevated regions.
continental-continental convergent margin
47
are characterized by horizontal motion along transform fault systems parallel to the boundary separating two plates form fault systems around the world
Transform plate boundaries
48
are part of curvilinear breaks in the seafloor known as _
fracture zones
49
home to landforms including continental rifts and oceanic ridges.
Divergent plate boundaries
50
gives rise to landforms known as continental volcanic arcs
Convergence
51
forms volcanic island arcs, or simply, island arcs.
oceanic-oceanic convergence,
52
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.
Continental-continental (C-C) convergence
53
are part of curvilinear breaks in the seafloor known as fracture zones.
Transform faults