vTHE INTERNAL STRUCTURE OF THE EARTH Flashcards

1
Q

describes the outermost shell of a terrestrial planet

part of a single geologic unit called the lithosphere

A

THE CRUST

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2
Q

mostly made up of igneous rocks, like granite and basalt

Our planet’s thin, 40-kilometer (25-mile) deep crust—just 1% of Earth’s mass—contains all known life in
the universe.

A

THE CRUST

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3
Q

Today, tectonic activity is responsible for the formation (and destruction) of crustal materials.

A

THE CRUST

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4
Q

Billions of years ago, the
planetary blob that would
become the Earth started out
as a hot, viscous ball of rock.

A

earth’s core

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5
Q

The molten material
that surrounded the
core was the early

A

mantle

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6
Q

The heaviest material,
that sank
to the center of the new
planet and became its core.

A

iron and nickel

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7
Q

Over millions of years, the
mantle cooled. Water
trapped inside minerals
erupted with lava, a
process called

A

“outgassing.”

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8
Q

Materials that initially stayed in
their liquid phase during this
process, called _______ ultimately became
Earth’s brittle crust.

A

“incompatible
elements,”

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9
Q

TWO TYPES OF CRUST

A

Continental Crust
Oceanic Crust

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10
Q

The transition zone between these two
types of crust

A

Conrad discontinuity

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11
Q

Conrad discontinuity

named after the seismologist

A

Victor
Conrad

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12
Q

are the most abundant
rocks and minerals in both oceanic
and continental crust

A

Silicates

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13
Q

(mostly compounds made of silicon
and oxygen)

A

Silicates

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14
Q

mostly composed of different types of granites. Geologists often refer to the rocks of the
continental crust as “sial”

A

CONTINENTAL CRUST

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15
Q

made up of silicate and aluminium

  • the most abundant elements
A

Sial

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16
Q

created by plate tectonics

A

CONTINENTAL CRUST

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17
Q

where tectonic plates crash into each other, continental crust is thrust up in the process of orogeny, or mountain-building.

A

convergent plate boundaries,

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18
Q

the thickest parts of continental crust are at the

A

world’s tallest mountain ranges.

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19
Q

the crust extends unevenly below the Earth as well as soaring into the atmosphere

A

CONTINENTAL CRUST

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20
Q

the oldest and most stable part of the continental
lithosphere

usually found deep in the interior of most
continents

A

Cratons

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21
Q

2 Types of Cratons

A

Shields

Platforms

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22
Q

cratons in which the ancient basement
rock crops out into the atmosphere

23
Q

are cratons in which the basement rock is
buried beneath overlying sediment

24
Q

is almost always much older than the
oceanic crust. Because continental crust is rarely destroyed and
recycled in the process of subduction, some sections of
continental crust are nearly as old as the Earth itself.

A

continental crust

25
Extending 5-10 kilometres beneath the ocean floor Mainly composed of basalts The rocks are often refer as “sima”
OCEANIC CRUST
26
made up of silicate and magnesium - the most abundant minerals in the crust
Sima
27
Denser than the continental crust Constantly formed at mid-ocean ridges, where tectonic plates are tearing apart from each other Destroyed at subduction zones
OCEANIC CRUST
28
the ___ and _____ of oceanic crust increases with distance from mid-ocean ridges.
age and density
29
important geologic process in which a tectonic plate made of dense lithospheric materials melts or falls below a plate made of less-dense lithosphere at a convergent plate boundary
Subduction
30
Mostly solid bulk of Earth’s interior Lies between Earth’s dense, superheated core and its thin outer layer, crust Makes the 84% of the Earth’s total volume
THE MANTLE
31
2 types of TEMPERATURE in the mantle
Near boundary between crust Near boundary with the core
32
- Varies from 1000 degrees Celsius
Near boundary between crust
33
- 3,700 degrees Celsius
Near boundary with the core
34
4 TYPES OF ROCKS
Olivine Garnet Pyroxene Magnesium oxide
35
Mostly silicates (a wide variety of compounds that share a silicon and oxygen
TYPES OF ROCKS in the mantle
36
5 ELEMENTS FOUND IN THE MANTLE
Iron Aluminum Calcium Sodium Potassium
37
Extends from the crust to a depth of about 410 kilometres Mostly solid, but its more malleable regions Contributes to tectonic activity
THE UPPER MANTLE
38
TWO PARTS OF THE MANTLE
Lithosphere Asthenosphere
39
The division between the crust and the mantle
THE MOHOROVICIC DISCONTINUITY
40
THE MOHOROVICIC DISCONTINUITY Simply called as
Moho
41
THE MOHOROVICIC DISCONTINUITY Named after Croatian seismologist
Andrija Mohorovicic
42
Who first detected in 1909 by examining the seismic waves moving through the Earth
Andrija Mohorovicic
43
Is the solid, outer part of Earth Includes both crust and the brittle upper portion of the mantle Both the coolest and the most rigid of Earth’s layers
LITHOSPHERE
44
Tectonic Activity is found in
LITHOSPHERE
45
Describes the interaction of the huge slabs (flat, thick piece of material such as earth or stone) lithosphere called tectonic plates
Tectonic Activity
46
Denser, weaker layer beneath the lithosphere mantle Temperature and pressure are so high that rocks soften and partly melt, becoming semi-molten
ASTHENOSPHERE
47
More ductile than either the lithosphere or lower mantle More viscous than the lithosphere
ASTHENOSPHERE
48
The very slow motion of lithospheric plates
“floating”
49
is the cause of plate tectonics, continental drift, earthquakes, the formation
plates “floating”
50
One of the most obscure places in the world separates two continents and two tectonic plates, namely the North American and Eurasian plates.
THE SILFRA RIFT
51
THE SILFRA RIFT divides two tectonic plates namely
North American and Eurasian plates.
52
hotter and denser than the upper mantle much less ductile than the upper mantle intense pressure keeps the lower mantle solid
THE LOWER MANTLE
53
responsible for transferring heat from the inner and outer core to the upper layers of the planet
THE LOWER MANTLE