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New Zealand is a country with a high rate of tectonic activity, such that earthquakes are an ever-present hazard across much of the country. In South Island the most important geological structure is the Alpine Fault, which runs for about 500 km along the west side of the mountain chain before splitting into a series of faults (known as the Marlborough fault system) that cross the northern part of the land mass (image from the University of Otago):
The recent 7.1 earthquake in Canterbury, New Zealand has reportedly caused damage to 100,000 homes amongst a range of other problems in the South Island. Dave Petley, a researcher with IHRR and Durham University is currently in New Zealand attending a conference and is reporting on the size and magnitude of the earthquake from his blog. More than 80 aftershocks have been recorded, according to the BBC. There is concern from the public and scientists alike that they could experience another earthquake in the very near future. Earthquakes are generally not new to New Zealand, but it is unusual for the country to experience an earthquake of this magnitude. GeoNet, a geological hazard monitoring system in New Zealand, provides a list of the largest earthquakes that have occurred historically in New Zealand that gives some idea of when and where they occur: http://www.geonet.org.nz/earthquake/historic-earthquakes/ Read more




