Story: Earthquakes

The earthquake magnitude scale (2nd of 2)

The earthquake magnitude scale

The magnitude scale measures the size of an earthquake at its source. This measurement is taken from a seismogram, using two variables. One is the time between the arrival of the primary (P) and secondary (S) waves ­the S-P time (secondary minus primary). It indicates the distance from the origin or focus of the earthquake, under the ground. The other variable is the height of the biggest wave (amplitude). A line can then be drawn between these measurements on a chart known as a nomogram. This has an S-P scale on one side and an amplitude scale on the other, and the intersection of a line joining the two values with the magnitude scale indicates the size of the earthquake. In the example shown here, the S-P time is 24 seconds, and the amplitude is 23 millimetres, giving a magnitude of 5. A magnitude 9 quake is extremely rare.

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How to cite this page:

Eileen McSaveney, 'Earthquakes - What causes earthquakes?', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/en/diagram/4404/the-earthquake-magnitude-scale (accessed 14 December 2019)

Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 1 Aug 2017