The Alpine Fault is sometimes compared with California’s San Andreas Fault, being another fast-moving strike slip fault near a plate boundary. However, its long term behaviour is unknown. It is widely recognised that the pioneering work of Harold Wellman, a surveyor, geologist, gold miner and intrepid explorer, revealed the large plate boundary fault in the South Island of New Zealand – the Alpine Fault. More exactly, the Alpine Fault. 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. This diagram shows the South Island of New Zealand. The Alpine fault is a plate boundary that cuts across the land in a northeasterly- southwesterly direction. By the end of this activity, students should be able to: understand the movement of plate boundaries in different parts of New Zealand. This activity was developed for the Earthquake Commission (EQC) and The Alpine Fault is a transform boundary between the Pacific Plate and the Indo-Australian Plate. 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 fault moves at about 26 mm … 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! Find out how it was discovered and learn what science can tell us about Alpine Fault earthquakes. The research team drilled to a depth of 893 m directly into the active Alpine Fault in Whataroa, New Zealand. I am at the south island of New Zealand! Recent field investigations revealed a unique opportunity to develop a long earthquake record for the Alpine Fault. The fault line is where the Eurasian and … 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 runs right through the heart of New Zealand's glacier county on the country's south island. plate boundaries under the North and South Islands representing the North Island subduction zone and the South Island Alpine Fault. Gold was discovered in distinctive rocks near Queenstown on the southeast side of the fault. 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. Strike slip Fault near a plate boundary the research team drilled to a depth of 893 m into! 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