I am at the south island of New Zealand! More exactly, the Alpine Fault. Recent field investigations revealed a unique opportunity to develop a long earthquake record for the Alpine Fault. This activity was developed for the Earthquake Commission (EQC) and Find out how it was discovered and learn what science can tell us about Alpine Fault earthquakes. This diagram shows the South Island of New Zealand. The fault moves at about 26 mm … New Zealand’s own major, plate boundary fault – the Alpine Fault – is one of the fastest slipping faults in the world and is known to rupture in large earthquakes. The Alpine fault, and its transition to the Marlborough Fault System in the northern South Island of New Zealand, offer such an opportunity using late Holocene geologic slip rates and vectors to assess an important on-land transitional plate boundary. plate boundaries under the North and South Islands representing the North Island subduction zone and the South Island Alpine Fault. By the end of this activity, students should be able to: understand the movement of plate boundaries in different parts of New Zealand. Gold was discovered in distinctive rocks near Queenstown on the southeast side of the fault. Revised slip rates for the Alpine fault at Inchbonnie: Implications for plate boundary kinematics of South Island, New Zealand May 2010 Lithosphere 2(3):139-152 The Alpine Fault is a geological fault, known as a right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island. The Alpine fault is a plate boundary that cuts across the land in a northeasterly- southwesterly direction. Take a tour along the Alpine Fault, Aotearoa New Zealand’s on-land plate boundary and one of the longest natural straight lines in the world! The research team drilled to a depth of 893 m directly into the active Alpine Fault in Whataroa, New Zealand. However, its long term behaviour is unknown. 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