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 1º
The Earth is divided into layers:
 The crust is the surface layer. It is a thin,
solid layer made of rock. The Earth’s crust
has a solid part (continents), and a liquid
part (oceans).
 The mantle is the intermediate layer. This
layer is almost 85 % of the Earth’s volume. It
includes magma, which is molten rock.
 The core is the deepest layer.
 In 1912, Alfred Wegener outlined his
continental drift theory. According to this
theory 200 millions years ago there was a
single giant land mass (one supercontinent),
called Pangaea. This Pangaea was
surrounded by a single ocean, called
Tethys Sea.
 The Pangaea broke up, forming the continents.
 These continents are no fixed, but they are
moving, because the crust (the Earth’s layer
where we live) is divided into several plates,
called tectonic plates.
 These plates are moving slowly over the mantle.
They move at a speed of 2 to 10 centimetres per
year.
 Some tectonic plates move apart, while
others collide.
 Where plates collide the Earth’s surface
often undulates and folds are created.
 The Earth’s crust sometimes fractures if the
surface where plates collide is extremely
rigid. Then, faults are created, and blocks
rise or sink.
 The movement of tectonic plates can
produce volcanoes and
earthquakes.
 A volcano is an opening in the planet surface
or crust which allows hot magma to
escape. When magma comes out of a
volcano, it is called lava.
 When a volcano erupts, it also ejects ash
and gases.
 Volcanic eruptions under the sea can form
islands such as the Canary Islands.
 Magma is pushed up
by the Earth’s internal
forces.
 It rises through a pipe
or a vent.
 It comes out through a
crater.
 Volcanic cones are
the result of lava
accumulating outside
the opening.
 When two tectonic plates crash, there is a
release of energy that makes the ground
vibrate. This vibration is called an
earthquake or seism.
 The vibration can be very violent or almost
unnoticeable.
 If an earthquake occurs on the ocean floor
can produce huge waves called
tsunamis.
 There are about half a million earthquakes
each year, but only about a thousand cause
any serious damage.
 During an earthquake the shock waves
spread out from a point below the surface
that is called the focus. The point at ground
level, directly above the focus, is called the
epicentre.
 The Richter scale and Mercalli scale are
both used to measure the strength of a
quake.
On the Earth’s crust there are emerged and
submerged lands:
Continents occupy 30% of the land
surface and are surrounded by oceans and
seas. There are six continents: Asia,
America, Africa, Antarctica, Europe
and Australia.
 Most of the emerged land is in the northern
hemisphere.
Oceans are large masses of salt water.
There are five oceans: The Pacific Ocean,
The Atlantic Ocean, The Indian Ocean,
The Arctic Ocean and the Southern
Ocean.
 Most oceans are in the southern hemisphere.
 The Earth’s surface isn’t flat, there are
mountains, plains, plateaux, valleys, etc. The
relief of the continents is very diversed.
 The relief is the result of the internal
forces of the Earth(plate movements,
volcanoes, earthquakes, etc.) and external
agents (wind, rain, temperature, rivers,
waves, ice... and human-beings).
The earth’s relief
The earth’s relief
The earth’s relief

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The earth’s relief

  • 2. The Earth is divided into layers:  The crust is the surface layer. It is a thin, solid layer made of rock. The Earth’s crust has a solid part (continents), and a liquid part (oceans).  The mantle is the intermediate layer. This layer is almost 85 % of the Earth’s volume. It includes magma, which is molten rock.  The core is the deepest layer.
  • 3.
  • 4.  In 1912, Alfred Wegener outlined his continental drift theory. According to this theory 200 millions years ago there was a single giant land mass (one supercontinent), called Pangaea. This Pangaea was surrounded by a single ocean, called Tethys Sea.
  • 5.
  • 6.  The Pangaea broke up, forming the continents.  These continents are no fixed, but they are moving, because the crust (the Earth’s layer where we live) is divided into several plates, called tectonic plates.  These plates are moving slowly over the mantle. They move at a speed of 2 to 10 centimetres per year.
  • 7.
  • 8.
  • 9.  Some tectonic plates move apart, while others collide.  Where plates collide the Earth’s surface often undulates and folds are created.  The Earth’s crust sometimes fractures if the surface where plates collide is extremely rigid. Then, faults are created, and blocks rise or sink.
  • 10.
  • 11.
  • 12.  The movement of tectonic plates can produce volcanoes and earthquakes.
  • 13.  A volcano is an opening in the planet surface or crust which allows hot magma to escape. When magma comes out of a volcano, it is called lava.  When a volcano erupts, it also ejects ash and gases.  Volcanic eruptions under the sea can form islands such as the Canary Islands.
  • 14.  Magma is pushed up by the Earth’s internal forces.  It rises through a pipe or a vent.  It comes out through a crater.  Volcanic cones are the result of lava accumulating outside the opening.
  • 15.  When two tectonic plates crash, there is a release of energy that makes the ground vibrate. This vibration is called an earthquake or seism.  The vibration can be very violent or almost unnoticeable.  If an earthquake occurs on the ocean floor can produce huge waves called tsunamis.
  • 16.  There are about half a million earthquakes each year, but only about a thousand cause any serious damage.  During an earthquake the shock waves spread out from a point below the surface that is called the focus. The point at ground level, directly above the focus, is called the epicentre.  The Richter scale and Mercalli scale are both used to measure the strength of a quake.
  • 17.
  • 18. On the Earth’s crust there are emerged and submerged lands: Continents occupy 30% of the land surface and are surrounded by oceans and seas. There are six continents: Asia, America, Africa, Antarctica, Europe and Australia.  Most of the emerged land is in the northern hemisphere.
  • 19. Oceans are large masses of salt water. There are five oceans: The Pacific Ocean, The Atlantic Ocean, The Indian Ocean, The Arctic Ocean and the Southern Ocean.  Most oceans are in the southern hemisphere.
  • 20.
  • 21.
  • 22.  The Earth’s surface isn’t flat, there are mountains, plains, plateaux, valleys, etc. The relief of the continents is very diversed.  The relief is the result of the internal forces of the Earth(plate movements, volcanoes, earthquakes, etc.) and external agents (wind, rain, temperature, rivers, waves, ice... and human-beings).