However, its long term behaviour is unknown. Recent field investigations revealed a unique opportunity to develop a long earthquake record for the Alpine Fault. Find out how it was discovered and learn what science can tell us about Alpine Fault earthquakes. 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 fault line is where the Eurasian and … By the end of this activity, students should be able to: understand the movement of plate boundaries in different parts of New Zealand. 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. This activity was developed for the Earthquake Commission (EQC) and More exactly, the Alpine Fault. The Alpine Fault is a transform boundary between the Pacific Plate and the Indo-Australian Plate. The Alpine fault is a plate boundary that cuts across the land in a northeasterly- southwesterly direction. 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. plate boundaries under the North and South Islands representing the North Island subduction zone and the South Island Alpine Fault. The Alpine Fault is sometimes compared with California’s San Andreas Fault, being another fast-moving strike slip fault near a plate boundary. 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