ertsay Flashcards

1
Q

The ____ states ocean being that crust formed at mid-ocean ridges and destroyed at deep-sea trenches”.

A

Sea floor
spreading theory

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

is a geologic
process of the movement of two oceanic
plates, splitting apart from each other at
a divergent plate boundary.

A

Seafloor spreading

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Seafloor spreading is a geologic
process of the movement of two oceanic
plates, splitting apart from each other at
a

A

divergent plate boundary.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

It results in
the formation of new oceanic crust from
magma that comes from within the

A

Earth’s mantle along a mid- ocean ridge.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

carry heat
from the lower mantle and core to the
lithosphere.

A

Convection currents

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Convection currents also
reutilize ___________ back to the mantle

A

lithospheric materials

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

As tectonic
plates gradually distance from each other, heat from the mantle’s convection
currents makes the crust more plastic and less dense. The less-dense material ______,
often forming a mountain or elevated area of the seafloor.

A

rises

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

As a result, the crust cracks. Hot magma powered by mantle convection
bubbles up to fill these fractures and spills onto the crust. This bubbled-up magma
is cooled by _________ to form igneous rock. This rock (basalt) becomes a new
part of Earth’s crust.

A

frigid seawater

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

As a result, the crust cracks. Hot magma powered by mantle convection
bubbles up to fill these fractures and spills onto the crust. This bubbled-up magma
is cooled by frigid seawater to form igneous rock. This _________ becomes a new
part of Earth’s crust.

A

rock (basalt)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

It is the process by which the ocean floor sinks beneath a deep-ocean
trench and back into the mantle, and allows part of the ocean floor to sink back
into the mantle.

A

Seafloor Spreading Subduction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

is the largest depression of land surface on Earth under an
ocean.

A

Ocean basin

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

happens along the boundaries of tectonic plates that
are moving apart from each other. These areas are called mid-ocean ridges.

A

Seafloor spreading

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

happens along the boundaries of tectonic plates that are
crashing into each other.

A

Subduction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

In these subduction zones, the __________ moves
underneath, or subducts, the ___________. Ocean basins that experience
subduction, such as the Pacific basin, are shrinking.

A

heavier plate, lighter one

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Oceanic basin landforms have two main characteristics namely:

A

1) Ocean
basin is a land that exists under an ocean; and 2) It includes all topographical
features.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

It is a shallow gently sloping part of the continental crust that borders the
continents. It has an average depth of 130 m, and its width varies from tens of
meters to a maximum of about 1, 300 km.

A

Continental shelf

17
Q

It extends from the continental shelf at an average depth of 135 meters.
The base is steeply sloping and occurs at a depth of approximately 2000 meters
that marks the edge of the continents. The width of the slope varies from 20 to 100
kilometers.

A

Continental slope

18
Q

The V-shaped canyon that cuts into the continental slope to a depth of up
to 1200 meters. It cuts perpendicular to the running direction of the continental
slope.

A

Submarine canyon

19
Q

It is found at the base of the continental slope. The depth ranges from 2000
to 5000 meters deep, and the width is up to 300 kilometers. Continental rise is
created by the merging of accumulated deposit at the mouth of the many
submarine canyons.

A

Continental rise

20
Q

It is the canyon’s thick fan-shaped sedimentary deposits.

A

Abyssal fan

21
Q

It is found at the base of the continental rise in water, ranging from 4 000 to
6 000 meters deep. Ocean floor accounts for nearly 30 % of the Earth’s surface,
consisting of thin layer of basaltic rock

A

Ocean floor

22
Q

This layer combines the rigid
crust plus the upper-most mantle.

A

Lithosphere:

23
Q

Partially molten part of
upper mantle. Tectonic plates are able to
move about on top of the softer, partially
molten asthenosphere.

A

Asthenosphere:

24
Q

The Core is at the center of the Earth. It is
divided into an inner and outer core.

A
25
Q

is the layer surrounding the
core.

A
  1. The Mantle
26
Q

is the rigid outermost layer

A
  1. The Crust, or lithosphere,
27
Q

The upper mantle is partially molten
and called the

A

asthenosphere.

28
Q

is a scientific theory which describes the large-scale motions
of Earth’s lithosphere.

A

Plate tectonics

29
Q

There are three types of plate movement:

A

the converging,
diverging or transversing against one another

30
Q

Folding is a tectonic activity that results in the formation of _________, such as the Himalayas,

A

Fold
Mountains

31
Q

is formed from faulting.

A

Rift Valley,

32
Q

are created when two continental crusts collide.

A

Mountain belts

33
Q

is also formed along the subduction zone.

A

Trench

34
Q

Divergence of ___________ occur mostly as mid-ocean ridges
where normal faults can be found.

A

plate boundaries

35
Q

divergence within _____________ leads to the formation of rift valleys.

A

continental
crusts

36
Q

form the strike-slip fault and frequent
earthquakes occur.

A

Transform plate boundaries

37
Q

Seafloor spreading happens along the boundaries of tectonic plates that
are moving apart from each other. These areas are called

A

mid-ocean ridges.