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GEOGRAPHY
Tectonics
Structure of earth
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Charlotte hansmeyer
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The earths surface is separated into
tectonic
plates
structure of the earth:
the centre: CORE
2 parts of the core: inner and
outer
Inner is a ball of
solid
iron and
nickel
Outer core is
liquid
Structure of the earth:
around the core:
MANTLE
made up of
semi-molten
rock that moves very slowly
structure of the earth:
on the top:
CRUST
10-70km
thick
Divided into slabs called
tectonic plates
that float on the
mantLe
2 types of crust:
continental
and
oceanic
oceanic crust is
thinner
and more
dense
continental crust is
thicker
and less
dense
Tectonic plates move due to
convection currents
in the
mantle
low parts of the mantle are hotter as they are
heated
by the
core
This makes it
less dense
as they heat up and rise
Move to the top of the mantle where is
cools down
and
sinks
Creates
circular movements
which move the tectonic plates