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Rocks

Igneous Rocks - History.

The Earth is about 4·6 billion years old (4,600,000,000 years).

The Earth was very hot and molten.
As it cooled, the first solid rock crust appeared about 4 billion years ago.
This solid crust (the first igneous rocks)
formed on the surface of molten magma.
Magma is a thick liquid molten rock (like treacle)
which can form within the mantle or the crust.

The mantle mainly contains hot solid rock
which can flow only very very slowly.
This slow movement makes sections (plates) of the crust collide
or slide past each other (see Plate Tectonics on the GCSE Physics site).
The enormous amount of energy which is released when plates collide
is sufficient to melt parts of the mantle or crust and form magma.
The magma can then solidify inside the crust (see granite)
or flow from a volcano and solidify on the surface of the crust (see basalt).

Structure of the Earth

At the centre of the Earth is the core, which is made of iron and nickel.
In the middle it is solid (the inner core).
Further out (the outer core) it is liquid, between the inner core and the mantle.

The oldest rocks are igneous rocks.
They are called igneous from the Latin ignis, meaning fire,
like ignite - set fire to.

The Earth's crust, oceans and atmosphere are the sources
of all raw materials from which everything we see around us is made.

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