{"id":486,"date":"2020-04-29T11:00:10","date_gmt":"2020-04-28T23:00:10","guid":{"rendered":"https:\/\/blogs.otago.ac.nz\/eqsci\/?page_id=486"},"modified":"2020-04-30T12:54:57","modified_gmt":"2020-04-30T00:54:57","slug":"image-gallery","status":"publish","type":"page","link":"https:\/\/blogs.otago.ac.nz\/eqsci\/image-gallery\/","title":{"rendered":"Image gallery"},"content":{"rendered":"

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Jono Griffin pointing to the interface of the Hyde Fault, represented by the juxtaposition of basement schist thrust over fine-grained silts and sands. Photo credit: Erin Todd, 2019.<\/p><\/div>\n

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Hyde Fault trench at the foot of the Rock and Pillar Range, looking southeast towards Taieri Ridge in the distance. Photo credit: Erin Todd, 2019.<\/p><\/div>\n

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Jono Griffin, Mark Stirling and the excavator operator overseeing an excavation across a fault trace associated with the NW Cardrona Fault. (Photo credit: Ella van den Berg, 2019).<\/p><\/div>\n

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The team preparing the Hundalee Trench for logging. The Hundalee Fault was one of 20+ faults that ruptured in the M7.8 2016 Kaik\u014dura earthquake. Left to right: Ella van den Berg, Kat Sauer (previously University of Otago), Jack Williams (Cardiff University), and David Barrell (GNS Science Dunedin). Photo credit: Mark Stirling, 2018.<\/p><\/div>\n