Wellington: New research has identified an active fault near New Zealand’s largest city, suggesting earthquake risk for Auckland may be higher than previously understood.
The Mangatangi Fault, running along the Hunua Ranges about 50 km south of the city, is capable of generating an earthquake of up to magnitude 6.8 said a press release by the University of Auckland on Wednesday.
“If the whole fault ruptured, there would likely be serious consequences for people living in South Auckland, and possibly further into central Auckland as well,” said geologist James Muirhead from the University of Auckland, the study’s co-author.
This is the first time a faultline in the Auckland region has been radiocarbon dated, highlighting limited knowledge of its seismic history, Muirhead said, adding that Auckland’s hazard “may be significantly higher than the public and policymakers believe.”
Auckland experiences earthquakes every year, but most are too small or distant to be noticed, he noted.
“This is an active fault with the potential to generate a large earthquake in a region that doesn’t expect one,” said Hannah Martin from the University of Auckland who was the lead author of the research, Xinhua news agency reported.
Earthquakes happen every day in New Zealand. Instruments record the ground shaking from over 20,000 earthquakes in and around the country each year. Most are too small to be noticed, but between 150 and 200 are big enough to be felt. Between 1840 and 2016, earthquakes in New Zealand caused 501 deaths directly or indirectly.
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