The Earth's Layers Flashcards

1
Q

What three layers is the inferior of the earth divided into

A

Crust, mantle and core

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2
Q

What is the core made up of

A

Dense rocks containing iron and nickel alloys

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3
Q

What is the core divided up into

A

A solid inner core and a molten outer one

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4
Q

What temperatures does the core reach

A

Over 5,000•c

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5
Q

What is the mantle made up of

A

Molten and semi molten rocks containing lighter elements (silicon, oxygen, aluminium, potassium and sodium)

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6
Q

How thick is the crust beneath the oceans

A

6-10 km thick

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7
Q

How thick is the crust beneath the continents

A

Up to 70km thick

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8
Q

What is the crust and the upper mantle divided into

A

The lithosphere and the asthenosphere

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9
Q

What is the lithosphere

A
  • consists of the crust and the rigid upper section of the mantle
  • 80-90 km thick
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10
Q

What is the lithosphere divided up into

A

Seven larger plates and several smaller ones

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11
Q

What are the two categories that plates are divided up into

A

Oceanic and continental- depending on the type of material from which they are made

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12
Q

What is below the lithosphere

A

The semi-molten asthenosphere, on which the plates float and move

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13
Q

How thick is the continental crust

A

30-70 km thick

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14
Q

How thick is the oceanic crust

A

6-10 km thick

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15
Q

How old is the continental crust

A

Over 1,500 million years

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16
Q

How old is the oceanic crust

A

Less than 200 million years

17
Q

How dense is the continental crust

A

2.6 (lighter)

18
Q

How dense is the oceanic crust

A

3.0 (heavier)

19
Q

What is the composition of the continental crust

A

Mainly granite; silicon, aluminium, oxygen (SIAL)

20
Q

What is the composition of the oceanic crust

A

Mainly basalt; silicon, magnesium, oxygen (SIMA)

21
Q

What do hotspots do

A

Generate thermal convection currents within the asthenosphere, causing magma to rise towards the crust, spread and cool (the circulation of magma moves the crustal plates).

22
Q

What is formed due to convection currents

A

New crust along the line of constructive boundaries within plates & older crust destroyed at destructive boundaries.