Plate Movement Flashcards

1
Q

Describe the core of the earth

A
Size of Mars 
Densest part of the planet 
Rocks rich in nickel and iron 
Two parts : semi molten outer core and a solid inner core 
Temperature 5000c
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2
Q

Describe the mantle of the earth

A
Surrounds core 
Mainly silicate rocks rich in iron and magnesium
Most is semi molten 
Up to 3800c 
Densities increase as you go down mantle
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3
Q

Describe the crust of the earth

A

Thinnest layer, coolest, less dense rock

Rich in silicon, oxygen, aliminium, potassium and sodium

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4
Q

What are the two types of crust

A

Oceanic crust

Continental crust

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5
Q

What’s oceanic crust

A

Thin layer, younger basalt rock known as sima ( Silica and magnesium)
Thickness - 5-10km

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6
Q

What’s continental crust

A

Thicker layer of older, lighter granite rocks (sial ( silica and aluminium) crust up to 70km thick

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7
Q

What’s Alfred wegeners theory (1912)

A

All continents were once joined in ancient supercontinent Pangea. At some point the land masses had drifted apart until they occupied their current position

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8
Q

Evidence for wegeners theory of continental drift

A
  • continental or jigsaw fit
  • geological evidence
    -climatological evidence
    Biological evidence
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9
Q

What is the continental or jigsaw fit evidence

A

Some continents seem to fit together if placed beside each other eg Africa and South America

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10
Q

What’s the geological evidence for wegeners theory

A

Rocks of the same age and type and formation found in SE Brazil and South Africa
Similar glacial deposits found in Antarctica and South America and India ( thousands of km apart )

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11
Q

What’s the climatological evidence for wegeners theory

A

Places as far apart as Antarctica,North America and the U.K. contain coal deposits of a similar age that were formed in tropical conditions. They are no longer in tropical conditions so must have drifted apart

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12
Q

What’s the biological evidence for wegeners theory

A

Similar fossil formations are found either side of the Atlantic.
Plant remains from humid swamps that later formed coal deposits have been found in India and Antarctica

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13
Q

What did Harry Hess do ( sea floor spreading)

A

Updated wegeners ideas. Examined crust either side of mid Atlantic ridge
Studied age of rocks on Atlantic Ocean floor he found the youngest in the middle and oldest nearest USA. New rocks still been formed in Iceland

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14
Q

Evidence for sea floor spreading

A

Look at crust either side of mid Atlantic ridge

Palaeomagnatism

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15
Q

What is palaeomagnatism - evidence of sea floor spreading

A

Study of changes in earths magnetic field (polarity. Earths magnetic field switches polarity.iron records record magnetic field. Rocks in ocean crust show alternating polarity.,magnetic stripes are mirrored across ridge suggest ocean crust spreading

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16
Q

What are convection currents

A

Slow moving thermal currents Hotspots heat lower mantle creating thermal currents rise and sink. This circulation of magma allows plates to move.

17
Q

Sea floor spreading means more crust is created so earth would get bigger? But it didn’t, why??

A

Parts of earths crust were being destroyed. On Pacific coast submarines found deep ocean trenches which were destroying crust as new crust was created. It did this by subduction and provided mechanism for drifting of continents

18
Q

Why are oceanic plates younger than continental

A

They are denser so can sink therefore are destroyed at ocean trenches and are continuously being formed at ocean ridges.
Continental plates won’t sink due to low density

19
Q

What is a constructive plate margin

A

Where two sections of crust move apart
Can be two sections of oceanic crust
Or oceanic and continental crust

20
Q

Process that happens at constructive margin with two oceanic plates

A

Crust weakens and cracks and magma pushed through gaps it cools and solidifies and forms submarine volcanoes. The pulling apart can form faults

21
Q

Process that occurs at constructive margin between oceanic and continental crust

A

Only occurs where there’s a convection cell . Continental crust heated by cell.over time crust cracks (vertical faults) and moves apart

22
Q

Landforms that happen in oceanic areas where plates move apart

A

Mid Oceanic ridges eg mid Atlantic ridge overall they have a total length of 60,000km on planet.
Transform faults cut along ridge,Middle of ridge forms deep valley
Underwater volcanoes erupt along mid ocean ridges.

23
Q

Landforms that can happen at constructive plate margins when oceanic and continental plates drift

A

Rift Valleys. Formed when lithosphere stretches causing it to fracture into sets of parallel faults.land between faults then collapses into deep wide value eg great African Rift Valley extends 4000km from Mozambique to Red Sea. Magma rise though gaps-volcano

24
Q

What happens at a destructive margin,what types are there

A

Two sections of crust move towards each other, can be:

  • oceanic -continental
  • continental -continental
  • oceanic -oceanic
25
Q

What happens at a destructive oceanic/continental margin

A

Deep sea trenches eg Peru-chile trench +8km deep
fold mountains ,
volcanoes,
earthquakes

26
Q

Landforms at destructive continental /continental margin

A

No volcanoes
Earthquakes can happen
Fold mountains eg the Himalayas

27
Q

Landforms at destructive oceanic / oceanic margin

A

Deep sea trenches - denser of two plates subducts
Earthquakes can be triggered and volcanic eruptions can take place underwater and create island arcs when submarine volcanoes emerge above water eg Mariana islands.

28
Q

How do island arcs form

A

Two oceanic plates converge ocean trench forms.volcano forms and lava piles up on ocean floor until a submarine volcano rises above sea level to form island volcano. Typically strung out in curved chains - island arcs

29
Q

How does magma that forms island arcs form

A

Produced by partial melting of defending plate in subduction and or overlying lithosphere

30
Q

What is a conservative plate margin eg San Andreas fault system

A

Where two plates slide past each other. Pressure builds up as they rub and jolts. Can cause faults and earthquakes. One plate can move faster than the other
Eg Christchurch earthquake 2011

31
Q

How do fold mountains form at destructive continental/continental margins eg the ALPS

A

Continental plates crust is Lower density so not much subduction. As plates move towards each other edges and sediment between them forced up into fold mountains. Movement of plates trigger shallow focus earthquakes. Material can also be forced downwards

32
Q

What are hotspots

A

Localised area of concentrated radioactive elements inside the mantle they occur at Hawaiian islands
Don’t occur at plate boundaries

33
Q

What happens at a hotspot

A

A plume of magma can rise and eat into plate above.where lava breaks through surface it cools and solidifies over time and active volcanoes can occur above hotspots

34
Q

Landforms that occur at hotspots

A

Hotspots are stationary and as Pacific plates move over it a line of volcanoes is created called and island chain.volcano above hotspot is active and others extinct. Seeing the age of volcanoes in a line supports Alfred wegners plate movement theory .

35
Q

What will happen over a very long period of time to old Volcanoes in island chains et Hawaiian islands

A

Pressure on crust and marine erosion extinct volcanoes will eventually sink below sea level