Macquarie Island is an island in the southwestern Pacific Ocean, about halfway between New Zealand and Antarctica.
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Macquarie Island is an island in the southwestern Pacific Ocean, about halfway between New Zealand and Antarctica.
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Macquarie Island claimed Macquarie Island for Britain and annexed it to the colony of New South Wales in 1810.
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Macquarie Island had status as a biosphere reserve under the Man and the Biosphere Programme from 1977 until its withdrawal from the program in 2011.
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On 5 December 1997, Macquarie Island was inscribed on the UNESCO World Heritage List as a site of major geoconservation significance, being the only place on earth where rocks from the earth's mantle are being actively exposed above sea-level.
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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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The island lies close to the edge of the submerged continent of Zealandia, but is not regarded as a part of it, because the Macquarie Ridge is oceanic crust rather than continental crust.
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Macquarie Island is one of the cloudiest places on Earth with an annual average of only 856 hours of sunshine.
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Macquarie Island has five principal vegetation formations: grassland, herbfield, fen, bog and feldmark.
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So-called "Upland Seals" once found on Antipodes Islands and Macquarie Island have been claimed by some researchers as a distinct subspecies of fur seals with thicker furs, although it is unclear whether these seals were genetically distinct.
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Royal penguins and Macquarie Island shags are endemic breeders, while king penguins, southern rockhopper penguins and gentoo penguins breed here in large numbers.
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Macquarie Island ecology was affected by the onset of European visits in 1810.
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On 8 April 2014 Macquarie Island was officially declared pest-free after seven years of conservation efforts.
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