Macquarie Fault Zone in the context of "Australian plate"

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⭐ Core Definition: Macquarie Fault Zone

The 1,600 kilometres (990 mi) long Macquarie fault zone (also known as the Macquarie Ridge, its gazetted name since 2015, the Macquarie Ridge complex or historically as the Macquarie Fault) is a major right lateral-moving transform fault along the seafloor of the south Pacific Ocean which runs from New Zealand southwestward towards the Macquarie triple junction. It is also the tectonic plate boundary between the Australian plate to the northwest and the Pacific plate to the southeast. As such it is a region of high seismic activity and recorded the largest strike-slip event on record up to 23 May 1989, of at least Mw8.0

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Macquarie Fault Zone in the context of Macquarie Island

Macquarie Island is a subantarctic island in the south-western Pacific Ocean, about halfway between New Zealand and Antarctica. It has been governed as a part of Tasmania, Australia, since 1880. It became a Tasmanian State Reserve in 1978 and was inscribed as a UNESCO World Heritage Site in 1997.

Macquarie Island is an exposed portion of the Macquarie Ridge and is located where the Australian Plate meets the Pacific Plate.

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