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5th Year
Chapter 3- Earthquakes
Earthquake- Plate tectonic
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Earthquakes are
tremors
or
vibrations
in the earth's crust.
Earthquakes
are caused by the movement of the worlds
plates.
The Theory of
Plate Tectonics
tells us how the earth's crust is split into a number of sections called
plates.
Plates float on the
semi-molten
rock of the
mantle.
Convection
currents in the mantle cause the
magma
to rise, cool, flow sideways and
sink.
As a result the plates which float in the
mantle
are constantly
moving.
Earthquake activity is associated with the following plate boundaries:
Destructive
Boundaries
Conservative
Boundaries
Constructive
Boundaries
At
destructive
boundaries two plates
collide.
The heavier plate will be
subducted
(
sink
and
melt
).
The sinking plate in
destructive
boundaries may
jam
or
stick
resulting in a huge build up of
pressure.
Eventually the
destructive
plates may pull apart at a point in the earth's crust known as the
focus.
Seismic (shock) waves will radiate out from the focus causing
tremors
in the earth's crust.
The tremors will have most effect at the
epicentre
a point directly above the
focus.
Earthquakes at
destructive
boundaries can be divided into 2 groups:
Earthquakes associated with
fold
mountain building
Earthquakes associated with
subduction
The Japanese
Tsunami
quake in
2011
occurred at a
subduction
zone.
The
Pacific
plate was subducted resulting in an earthquake measuring
9.0
on the
Richter
Scale in the
Japanses
earthquake
The Japanese earthquake triggered a
Tsunami
which killed approximately
27,000
people.
Earthquakes also occur where two continental plates
collide
and
fold
mountains are formed.
The
Himalayas
formed as a result of the collision of the
Indian
and
Eurasian
plates and this area experiences
earthquake
activity.
Shallow earthquakes are associated with continental-continental
collision
The focus is less than
70
km deep with
continental-continental
collisions
quakes that make
fold
mountains are among the most
destructive
as their focus is so
close
to the surface.