SOUTH AMERICA
General Geological Setting
PLATES ARE DESTROYED (SUBDUCTION):
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This is a convergent plate boundary, the plates move towards
each other.
The amount of crust on the surface of the earth remains relatively
constant. Therefore, when plates diverge (separate) and form
new crust in one area, the plates must converge (come together)
in another area and be destroyed. An example of this is the Nazca
plate being subducted under the South American plate to form the
Andes Mountain Chain.
Here we can see the oceanic plate moving from left to right.
The top layer of the mantle and the crust (all called the lithosphere)
sinks beneath the continent. A deep ocean trench is formed.
Water gets carried down with the oceanic crust and the rocks begin
to heat up as they travel slowly into the earth. Water is then driven off
triggering the formation of pools of molten rock which slowly rises.
The plate moves downwards at a rate of a few centimetres per year.
The molten rock can take tens of thousands of years to then either:
 Solidify slowly underground as intrusive igneous rock
 such as granite .
 or
 Reach the surface and erupt as lava flows. Cooling rapidly to
form extrusive igneous rock such as basalt.
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The floor of the Easter Pacific is moving towards South America at
a rate of 9 centimetres per year. It might not seem much but over
the past 10 million years the Pacific crust has been subducted under
South America and has sunk nearly 1000 kilometres into the Earth's
interior.
EARTHQUAKES
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