In New Zealand, magnitude given to an earthquake is usually a summary magnitude, which is a combination of several different magnitude types that can be estimated most quickly.
“The different magnitude types and the different networks of other agencies provide important perspective on earthquakes in New Zealand,” a statement from GeoNet said.
“If you click on the ‘technical’ tab on an earthquake, (on the GeoNet website) you will see the different magnitudes used.
“Faults that could create earthquakes range in size from less than a metre long to more than 1000 kilometres for the largest earthquakes, and therefore the size of earthquake signals, how far they travel, and how well they are detected vary significantly. Because of this huge range, there is no one way to measure the magnitude of an earthquake that will capture all earthquakes. Seismologists have developed several ways to measure different aspects of an earthquake (different magnitude scales) which allows them to get the best idea of the size of the event and to be able to make direct comparisons with the magnitudes put out by other agencies.
“For large earthquakes ,seismologists use a particular magnitude scale called ‘moment magnitude’ (Mw). This scale measures the low frequency part of the signal and will continue to get larger regardless of how big the earthquake is.
“Moment magnitude is more difficult to calculate as it involves more than simply measuring the size of the signal at a certain frequency and requires a longer portion of the signal. Typically, it will take 20-30 minutes to calculate a reliable moment magnitude which is why it is released later, but it is considered the most reliable magnitude for the largest earthquakes.”