SCIENCE 1st summative Flashcards

1
Q

the seafloor was formed by
mid-ocean ridges that
spread in both directions.

A

Seafloor Spreading Theory

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2
Q

geologic process that takes place
when tectonic plates diverge,
resulting in the creation of new
ocean floors.

A

Seafloor Spreading Theory

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3
Q

an American geologist,
professor, and military officer,
proposed the seafloor spreading
theory in 1960s.

A

Harry Hess

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4
Q

a scientist with the US coast and
Geodetic Survey, coined the term
“seafloor spreading”

A

Robert S. Dietz

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5
Q

are areas
where tectonic plates dive
beneath other plates into
the earth’s interior.

A

Subduction zones

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6
Q

It occurs when two plates push
against each other. While one plate
dives beneath another, the crust is
destroyed and recycled back into
the earth’s interior.

A

(Colliding Boundary)

Convergent

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7
Q

this boundary also known as the
destructive plate boundary.

A

(Colliding Boundary)

Convergent

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8
Q

____________________________ ________________ boundaries
occur when two continental plates move towards
each other. Both plates are less dense, so neither
subducts under the other. Instead, the plates
collide and push upwards forming large mountain
ranges.

A

Continental-to-continental
convergent

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9
Q

When oceanic crust collides with a continent, an
_____________________________________ _____________boundary forms.
The oceanic plate is denser, so it undergoes
subduction. This means that the oceanic plate sinks
beneath the continent, forming a deep ocean trench

A

Oceanic-to-continental
convergent

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10
Q

occurs location where two oceanic plates
come together and the denser plate
sinks, or subducts, beneath the less
dense plate, forming a deep ocean trench

A

Oceanic-to-oceanic

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11
Q

unlike the two boundary types, _________ _____neither creates nor destroys a crust,
hence it is also called conservative boundary

A

(Lateral Boundary)

Transform Fault

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12
Q

is a zone
where two lithospheric plates
move apart from each other.

A

A divergent boundary

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13
Q

this boundary also known as the
constructive plate boundary.

A

(Spreading Boundary)

Divergent

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14
Q

What really is
inside the Earth?
Mechanically

A

Lithosphere,
Asthenosphere, Mesospheric mantle,
Outer core, and Inner core.

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15
Q

The structure of Earth can be defined

A

mechanically or chemically.

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16
Q

is the study of the flow of matter
primarily in the liquid state under
conditions at which they respond with
plastic flow rather than deforming
elastically in response to an applied
force.

A

RHEOLOGY

17
Q

is the outermost layer of the Earth.

A

CRUST

18
Q

The earth is divided into three main layers namely the

A

Crust, the mantle and the core.

19
Q

What really is
inside the Earth? Chemically:

A

Crust, Upper Mantle, Lower
Mantle, Outer Core, and Inner Core.

20
Q

it is the thinnest layer, ranging from about 5 to 70 kilometers in thickness.

A

CRUST

21
Q

is the thicker layer of the Earth’s crust that is found under the continents. It is about 35 kilometers thick on average.

A

continental crust

22
Q

is the thinner layer of the Earth’s crust that is found under the ocean basins. It is about 7 kilometers thick on average.

A

oceanic crust.

23
Q

The crust can be further divided into two types

A

continental crust and oceanic crust.

24
Q

The mantle can be divided into an

A

upper and lower layer.

25
Q

It is the thickest layer, extending from the base of the crust to a depth of approximately 2,900 kilometers.

A

MANTLE

26
Q

is the layer beneath the Earth’s crust.

A

MANTLE

27
Q

Is seen as a
highly viscous layer which lies
between the crust and the
lower mantle.

A

The upper mantle

28
Q

extends
from just under the upper
mantle to 2,200 km.

A

The lower mantle

29
Q

is the innermost layer of the Earth, situated beneath the mantle.

A

CORE

30
Q

Rocks at the _______ _______are hot and soft.

A

LOWER MANTLE

31
Q

Rocks in the _______ _______ are cooler and brittle enough to break under
stress.

A

UPPER MANTLE

32
Q

It is divided into two distinct regions

A

the outer core and the inner core.

33
Q

represents
about 4% of the mantle-crust
mass.

A

OUTER CORE

34
Q

can be found at the
deepest region of the planet.

A

INNER CORE

35
Q

It can be regarded as a
ball of very hot metals.

A

OUTER CORE

36
Q

It is
characterized by an extremely high
temperature of about 5,000-6,000
degree Celsius or even higher than the
temperature at the sun’s surface

A

INNER CORE