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Geography

Earthquakes

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Earthquakes are caused by the release of built-up pressure inside the Earth's crust. An earthquake's power is measured on the Richter scale [Richter Scale: A logarithmic scale used to measure the impact of an earthquake by measuring the amount of energy it generates. ] using an instrument called a 'seismometer'.

The effects of an earthquake can be devastating - they can destroy settlements, change landscapes, and cause many deaths.

Causes

An earthquake is the shaking and vibration of the Earth's crust due to movement of the Earth's plates (plate tectonics). Earthquakes can happen along any type of plate boundary.

Earthquakes occur when tension is released from inside the crust. Plates do not always move smoothly alongside each other and sometimes get stuck. When this happens pressure builds up. When this pressure is eventually released, an earthquake tends to occur.

The point inside the crust where the pressure is released is called the focus. The point on the Earth's surface above the focus is called the epicentre.

Earthquake energy is released in seismic waves. These waves spread out from the focus. The waves are felt most strongly at the epicentre, becoming less strong as they travel further away. The most severe damage caused by an earthquake will happen close to the epicentre.

Diagram of an earthquake

Diagram of an earthquake

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