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Volcanoes Factfile 
Volcanoes

How Volcanoes Are Formed

Most people when asked to describe a volcano will describe a cone shaped mountain, with lots of fire and smoke spurting out of. But volcanoes aren't that simple as they come in different shapes, with the ability to explode with clouds of gas, steam and ash.

Our planet is made up of 3 layers - the Core, the Mantle and the Crust. (If you imagine our Earth as a hard-boiled egg, with a shell that has been cracked in places, this is a good comparison. The yolk represents the core, the egg white represents the mantle and the shell represents the Earth's crust).

The Earth's outer layer, the crust is broken into a number of sections called tectonic plates. These plates are enormous, the size of continents and they are constantly moving, floating on the magma in the mantle below. This movement is very slow (a few mm per year) and currents in the mantle, which keeps the magma moving, create the movement. The way these plates move is called Continental Drift and for most of the time, this movement happens without any negative consequence.

 
Plate Boundaries

1 - Indo-Australian Plate 8 - African Plate
2 - Antarctica Plate 9 - Europe/Asia Plate
3 - Nazca Plate 10 - Iranian Plate
4 - South American Plate 11 - Arabian Plate
5 - Cocos Plate 12 - Philippine Plate
6 - Caribbean Plate 13 - Pacific Plate
7 - North American Plate

However, these plates meet at plate boundaries or margins and any one of the following actions can provide the start for volcanic activity:
  • When two plates collide (converging plates) - As the two edges meet, one plate slides on top of the other, forcing the bottom plate down into the mantle. Here it melts into magma, which then forces its way up through cracks in the Earth's crust to form volcanoes. (When magma reaches the surface, it becomes known as `lava').
    Example: The volcanoes along the Pacific coast of South America.


    Converging plates - Lascar volcano - Dr P Francis

  • When two plates move away from each other (diverging plates) - As the two plates move away from each other, magma constantly rises up from the mantle to fill the opening, building up into an oceanic ridge or chain of underwater volcanoes.
    Example: The Mid-Atlantic Ridge. Some of these volcanoes reach above the sea as volcanic islands - the Azores, Tristan da Cunha, Surtsey (Iceland).


    Diverging plates - Tristan da Cunha

Other volcanoes are found in places known as `hot spots'. This is where a hole is made in the middle of a plate, where it is very thin and magma can force its way through from the mantle. Over millions and millions of years, the plate above the hot spot slowly moves over it, causing the volcano to die. But then a new volcano is created when another hole is made in the covering plate. This results in a chain of volcanoes very slowly being built up.
Example: the volcanic islands of Hawaii


Hot spots - Kahoolawe - Jack Lockwood

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Volcanoes Contents
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Types of Volcanoes
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How Big Are Volcanic Eruptions ?
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