Plate tectonics Flashcards

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1
Q

how old is the earth?

A

over 4.5 billion years old

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2
Q

what are the characteristics of the crust?

A

0-70km thick
coolest and least dense rocks
the rocks are rich in sodium, silicon, aliminium and potassium

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3
Q

what can the crust be divided into?

A

continental crust and oceanic crust

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4
Q

what are the characteristics of the continental crust?

A

its old
permanent
less dense

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5
Q

what are the characteristics of oceanic crust?

A

is young
can be created and destroyed
6-10 km thick
denser than continental crust

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6
Q

what are the characteristics of the mantle?

A

2900km thick
semi-molten rock
temperatures near core reach 5000 degrees
high temps generate convection currents

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7
Q

what are the characteristics of the core?

A
hottest part of the earth
over 5000 degrees
outer part is liquid
inner part is solid 
made from iron and nickle ore
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8
Q

what separates the mantle from the crust?

A

the mohorovicic boundary

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9
Q

the heat in the core is produced at a result of what 2 processes?

A

primordial heat

radiogenic heat

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10
Q

what is primordial heat?

A

left over heat from the earth’s formation

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11
Q

what is radiogenic heat?

A

produced by the radioactive decay of isotopes

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12
Q

what has the theory of plate tectonics helped us to understand?

A
  • the distribution of the worlds major landforms
  • where natural hazards can strike
  • the distribution of minerals and energy supplies
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13
Q

how do tectonic plates move?

A

convection currents

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14
Q

how do convection currents work?

A

heat is obtained by radioactive decay
hot air/liquid rises as it is less dense
cool air sinks as it is more dense

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15
Q

what is the hotspot theory?

A

wilson noted that in certain locations around the world volcanism has been active for very long periods of time
this could only happen if very small long lasting exceptionally hot regions called hotspots existed below the surface

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16
Q

how are hotspots formed?

A

radioactive decay within the core generates very hot temperatures.
if the decay is concentrated hot spots will form around the core
these hotspots heat the lower mantle creating localised thermal currents where magma plumes rise vertically

17
Q

what did wilson suggest about continuing plate movement?

A

Continuing plate movement eventually carries the island beyond the hotspot cutting it off from the magma source
as one island volcano becomes extinct another develops over the hotspot