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Earthquakes are the result of the formation of new faults within the lithosphere or the movement of older pre-existing faults.

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Faults are large fractures or cracks that form in the Earth's lithosphere. They can range in size from metres to 100's or 1000's of km.

Faults form within the lithosphere due to stress. As stress increases the lithosphere initially begins to deform elastically (like a spring being squashed or an elastic band being stretched). When the stress exceeds the strength of the lithosphere, a brittle failure occurs. Brittle failures are those where cracks or fractures form through the material. This releases all the energy stored in the rocks in one go as seismic waves causing an earthquake.

Now this has been going on for millions of years so that there are already a large number of fractures or faults in the lithosphere. These pre-existing points of weakness are now the first part of the lithosphere to fail when stress builds up.


they move up against each other.. constantly moving and the pressure gets to be too much and boom an earthquake happens.. islands are made by being pushed upward. it is a fascinating topic to read up on more

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