- published: 18 Feb 2013
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The Auckland metropolitan area ( /ˈɔːklənd/, AWK-lənd), in the North Island of New Zealand, is the largest and most populous urban area in the country with 1,377,200 residents, 31 percent of the country's population. Auckland has the largest Polynesian population of any city in the world. In Māori Auckland's names are Tāmaki Makaurau, and the transliterated version of Auckland, Ākarana.
The 2011 Mercer Quality of Living Survey ranked Auckland 3rd equal place in the world on its list, while the Economist's World's Most Livable Cities index of 2011 ranked Auckland in 9th place. In 2010, Auckland was classified as a Beta World City in the World Cities Study Group’s inventory by Loughborough University.
Auckland lies between the Hauraki Gulf of the Pacific Ocean to the east, the low Hunua Ranges to the south-east, the Manukau Harbour to the south-west, and the Waitakere Ranges and smaller ranges to the west and north-west. The central part of the urban area occupies a narrow isthmus between the Manukau Harbour on the Tasman Sea and the Waitemata Harbour on the Pacific Ocean. It is one of the few cities in the world to have harbours on two separate major bodies of water.
New Zealand (Māori: Aotearoa) is an island country located in the southwestern Pacific Ocean. The country geographically comprises two main landmasses ‒ that of the North and South Islands ‒ as well as numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island nations of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans.
During its long isolation, New Zealand developed a distinctive biodiversity of both animal and plant life. Most notable are the large number of unique bird species, many of which became extinct after the arrival of humans and introduced mammals. With a mild maritime climate, the land was mostly covered in forest. The country's varied topography and its sharp mountain peaks owe much to the tectonic uplift of land and volcanic eruptions caused by the Pacific and Indo-Australian Plates clashing beneath the earth's surface.
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