The structure of the Earth Flashcards

1
Q

How thick is the Earths crust on average?

A

20km thick

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2
Q

What is the lithosphere?

A

The crust and the upper/ rigid section of the mantle

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3
Q

What is the asthenosphere?

A

The upper part of the mantle (the boundary between the earths crust and mantle)

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4
Q

What causes the movement of plates?

A

convection currents

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5
Q

What is the outer core made up of?

A

molten iron and nickel

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6
Q

What is the inner core made up of?

A

solid iron and nickel

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7
Q

The cores temperature is over how many degrees celcius?

A

5000

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8
Q

What is primordial heat?

A

heat left over from the earths formation

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9
Q

What is radiogenic heat?

A

heat produced by radioactive decay of isotopes

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10
Q

Approximately how thick is the earths lithosphere?

A

approximately 80-90km thick

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11
Q

What is Mohorovicic Discontinuity?

A

semi-molten (plastic-like) rock that can move very slowly

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12
Q

How thick is oceanic crust?

A

6-10km thick

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13
Q

How thick is the continetial crust?

A

30-70km thick

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14
Q

Which is more dense oceanic or continential crust?

A

Oceanic

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15
Q

What crust can be subducted?

A

Oceanic

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16
Q

Which crust cant be renewed or destroyed?

A

Continential

17
Q

How old is the oceanic crust?

A

less than 2 million years

18
Q

How old is the continental crust?

A

over 1500 million years

19
Q

What is the oceanic crust made out of?

A

Basalt

20
Q

What is the continential crust made out of?

A

Granites/ sedimentary rock

21
Q

What crust moves faster?

A

Oceanic

22
Q

What are the rules for plate movement?

A

-Plates cant overlap
- No ‘gaps’ can occur on the surface
- As new crust is created, it must be destroyed somewhere else
-Very little change occurs in the middle of plates

23
Q

How quick is plate movement?

A

Very slow but continuous approximately 5-10 cm per year

24
Q

How do convection currents occur?

A
  • the earth core radiates heat so the semi-molten lower mantle becomes less dense
  • as a result it rises
  • then it drags the plates along due to friciton
  • eventually the magma cools and becomes denser
  • then the dense, cool magma sinks back to the core
  • this repeats