Photogrammetric reconstruction of the Alpine Fault outcrop at Gaunt Creek near Whataroa, New Zealand. Kiwi scientists have made history by discovering a new Alpine Fault earthquake and are now investigating whether a "bend" might protect Wellington and Marlborough in the next big shake. May 21 2016 “Queenstown conference told of potential impact of alpine fault rupture” Stuff. GNS details on the Alpine Fault The Alpine Fault, which runs for about 600km up the spine of the South Island, is one of the world’s major geological features. A companion set of longer videos provide more in-depth detail of the science underpinning ProjectAF8, which is funded by the Ministry of Civil Defence & Emergency Management and through the Resilience to Nature's Challenges Fund. AF8 [Alpine Fault Magnitude 8] is an award-winning programme of scientific modelling, response planning and community engagement designed to build a collective resilience and preparedness to the next Alpine Fault "We have used that scenario to work with our partners to identify the foreseeable impacts on communities and critical infrastructure across the South Island," he said. ProjectAF8 is a South Island-wide effort to co-ordinate planning and preparation for a severe earthquake on the fault. More work was being done to refine the date of that last quake. Studies at Alpine Fault excavation sites showed a large earthquake occurred on the fault every 300 years or so, with the last one occurring in 1717. The 2016 Kaikoura earthquake was a magnitude 7.8 (Mw) earthquake in the South Island of New Zealand that occurred two minutes after midnight on 14 November 2016 NZDT (11:02 on 13 November UTC). The southern part of the fault has been found to rupture on average every 291 years, plus or minus 23 years, and there is a 27 per cent chance of that happening again in the next 50 years. From the LEARNZ Alpine Fault online field trip… Scientists have established that the fault … (File photo). Video simulations demonstrate widespread destruction across the South Island if New Zealand's most dangerous fault line ruptures, and there's evidence the country is due for another big one. The four videos … Project Alpine Fault Magnitude 8 (AF8) released a series of videos on Wednesday, warning there's compelling geological evidence to show it produces a significant earthquake of … In Christchurch, the shaking from an Alpine Fault rupture might not feel as sharp as the February 2011 earthquake, Bradley said, but it would last a lot longer – about two or three minutes. Geologists and authorities are racing to quantify what might happen, and how they might respond in the event of the next one, likely to occur some time in the next 50 years. Ms Cooper lives near the Alpine Fault, which is likely to rupture within the lifetime of many New Zealanders. The Alpine Fault is the boundary between the Pacific crustal plate and the Australian plate. (File photo), Investigations of the Alpine Fault at Inchbonnie near the Taramakau River have been carried out by studying trenches dug across the fault and by using ground-penetrating radar. [2] Ruptures occurred on multiple faults and the earthquake has been described as the "most complex earthquake ever studied". The Alpine Fault ruptures—on average—every 330 years with a magnitude 8 earthquake. Howarth said 1740 was the earliest likely year for the recently discovered quake and it was unlikely to be much later than 1840, otherwise it would have been felt by South Islanders and talked about. The last rupture was believed to have happened in 1717. It's a puzzle. The slip rate here was much lower, only about 14mm a year, probably because movement was transferred in the northern section on to the Hope, Awatere and Wairau faults. The bend – where the fault turns from its northeast-southwest orientation to run in a more north-south direction – was a "big unknown" in terms of how it interfered with ruptures. They say it is too early to tell how their discovery may change the probabilities of when the next big, possibly magnitude 8-plus, Alpine Fault quake is due. Scientists question whether a 5.5 quake did indeed strike on the big-risk Alpine Fault. For their date discovery, Howarth and Langridge used new techniques of radiocarbon-dating to reanalyse organic material found in trenches on the section of the fault between the Toaroha River, about 20km southeast of Hokitika, and Springs Junction. The Alpine Fault is a geological fault that runs almost the entire length of New Zealand's South Island (c. 480 km) and forms the boundary between the Pacific Plate and the Indo-Australian Plate. Cows in front of the Alpine Fault scarp at Inchbonnie (file photo). Despite its obvious tectonic significance, the Alpine fault has not ruptured since European settlement in the 1840s. The geology of the West Coast of New Zealand's South Island is divided in two by the Alpine Fault, which runs through the Region in a North-East direction. The Alpine Fault, which runs up the spine of the South Island, has ruptured five times in the past 1100 years - producing an earthquake of between magnitude 7 … To the West of the fault Paleozoic basement rocks are interluded by plutones and both are unconformably covered in a sedimentary sequence. The two quakes they had found evidence for were the big quake in 1717 and the more recent quake, sometime between 1740 and 1840, he said. 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