Plate Tectonics Theory Flashcards

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1
Q

What are the 4 parts of the earth

A

Core (inner, outer)
Mantle
Crust

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2
Q

What is the inner core?

A

A solid ball made up of lots of iron and nickel

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3
Q

What is the outer core?

A

Semi-Molton, contains lots of iron and nickel

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4
Q

What is the mantle made up of

A

Silicate rocks - rocks that have loads of the element silicon in them

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5
Q

Characteristics of mantle

A
  • mantle nearest the core is quite rigid
  • layer above this is the asthenosphere - semi-Molton. Can flow
  • very top bit is very rigid
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6
Q

What is the outer layer of the earth called

A

Crust

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7
Q

What is the rigid top part of the mantle and the crust called

A

Lithosphere

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8
Q

Characteristics of continental crust

A

Thicker
30-70km thick
Less dense
2.7g/cm3 - density

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9
Q

Characteristics of oceanic crust

A

Thinner
6-10km
More dense
3.0g/cm3 - density

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10
Q

Lithosphere is divided into tectonic plates, why do they move

A

Convection currents in the asthenosphere

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11
Q

How do convection currents occur

A
  • radioactive decay of elements in mantle and core (uranium) generates a lot of heat
  • when lower parts of asthenosphere heat up, become less dense, slowly rise
  • as they rise to the top, they cool down, become more dense, then slowly sink
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12
Q

How do convection currents make the plates move

A

Create drag on the base of the tectonic plates (they’re solid and rigid) which causes them to move

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13
Q

When is new crust created

A

When plates move apart

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14
Q

Explain how new crust is created

A
  • convection currents move apart at the base of the lithosphere, causes plates to move apart
  • magma rises up to fill gap created, cools to form new crust
  • new crust is dragged apart and even more new crust forms between it
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15
Q

What happens to the sea floor when plates move apart under the sea

A

Spreads - sea floor spreading - gets wider

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16
Q

What structures are created when plates move apart under the sea

A

Mid-ocean ridges - ridges of higher terrain on either side of the margin

17
Q

who started the theory of plate tectonics

A

Alfred Wegner

18
Q

what made people think that there was once one big plate before they started to move apart

A

in 17th century people noticed South America and Africa looked like they could fit together

19
Q

In 1912, what theory did Alfred Wegener propose?

A

continental drift

20
Q

what did Wegener propose?

A

that all continents were once joined together as one super continent called Pangaea which drifted apart

21
Q

what did Wegener base his theory on?

A

geological evidence and fossil records

he couldn’t back it up with a mechanism that explained how the continents moved

22
Q

in the 1950s, what provided evidence for continental drift?

A

palaeomagnetism

23
Q

what provided a mechanism for continental drift

A

sea floor spreading - 1960s

24
Q

what are the 5 different categories that provide evidence for the theory of plate tectonics

A
  • geology
  • fossil records
  • living species
  • climatology
  • palaeomagnetism
25
Q

how has geology provided evidence for the theory of plate tectonics

A
  • areas of south america and Africa have rocks of the same age and composition
  • can match up the age, rock type and distribution of some mountain ranges e.g. mountains in Norway and Sweden
  • these rocks and mountains must’ve formed under the same conditions and in the same place in order to match so well - only possible if continents were once joined
26
Q

how has fossil records provided evidence for the theory of plate tectonics

A

-can match up the distribution of some fossils by fitting land masses together
unlikely that these species migrated across thousands of mile of water or that they evolved in different places
-fossil records suggest that these places were joined together when these organisms were alive

27
Q

how do living species provide evidence for the theory of plate tectonics

A
  • same living organisms can be found on different continents - unlikely for some to migrate across sea or to have evolved in different locations.
    e. g. earthworms found in New Zealand, Asia, North America
28
Q

how has climatology provided evidence for the theory of plate tectonics

A
  • evidence that the past climates of some continents were similar - once located together
    e. g. similar glacial deposits are found in antarctica, africa, india and australia. fitting places together, you can match up the distribution of deposits-suggests they were joined together
29
Q

What is palaeomagnetism? and what does it provide evidence for?

A

the study of the history of the earth’s magnetic field. sea floor spreading

30
Q

how often does the earth’s magnetic field reverse polarity?

A

once every 200,000 years

31
Q

how does palaeomagnetism provide evidence for the theory of plate tectonics?

A
  • magma erupts from mid-ocean ridges, magnetic minerals in molten rock align themselves with direction of earth’s magnetic field
  • once new crust has solidified, alignment is fixed
  • magnetic minerals in crust created in periods of normal polarity are aligned in opposite direction to those in periods of reverse polarity
  • creates alternating bands of magnetic stripes along seafloor
  • stripes show crust is getting older, the further away from a mid-ocean ridge you go - plates are moving apart