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36 Earth


Planet Earth is a dense, rocky ball about 12,750 km


(7,920 miles) across. It is one of eight planets circling our


local star, the Sun. The Earth is the only planet we know


that supports life. From space, its surface looks blue


and cool, but inside it is so hot that rock can melt.


IS THE EARTH THE SAME ALL THE WAY THROUGH?
Our planet is made of four main layers. The outer
layer is called the crust. Below is the mantle,
which is solid near the top and molten
below. Temperatures become hotter
near the Earth’s centre. The outer
core is a mass of molten rock.
The temperature of the inner
core is up to 4,700°C (8,492°F).

HOW WAS THE EARTH FORMED?
The Sun began to form around 5,000 million years
ago out of a cloud of whirling dust and gas in space.
As it formed, the Sun’s gravity gradually pulled the
dust and gas into lumps, which became the planets.
At first, the Earth was a ball of molten rock. Its
surface rock slowly began to cool and harden
around 4,200 million years ago.

1 EARTH’S STRUCTURE
The crust is made up of oceanic
crust, below the oceans, and
continental crust, which carries the Earth’s
land. It is the Earth’s thinnest layer, at only
6–70 km (4–43 miles) thick. The mantle, at 2,900
km (1,800 miles) deep, is the thickest layer. The outer
core is around 2,000 km (1,240 miles) thick. The inner core at
the centre of the Earth is about 2,740 km (1,702 miles) across.

YOUNG PLANET
Around 4,500 million years ago,
the young Earth was bombarded
from space by huge rocky
meteorites and asteroids. Molten
(liquid) rock from the Earth’s fiery
centre erupted from thousands
of volcanoes. As the Earth slowly
began to cool, clouds of gas and
water vapour escaped from cracks
in the crust (the planet’s thinner,
outer layer) and formed the first
atmosphere. The water vapour
eventually formed the oceans.

EARTH’S ATMOSPHERE
The Earth’s atmosphere is a
layer of gases about 700 km
(430 miles) thick. Without the
atmosphere there could be no
life on the Earth. It protects us
from harmful rays in sunlight,
and prevents the Earth from
becoming too hot or too cold.

PLANET EARTH


Solid inner core
of white-hot
nickel and iron

Atmosphere

Crust

Molten
outer core

Mantle

Planet Earth

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