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Portal:New Zealand

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New Zealand
Aotearoa (Māori)
A map of the hemisphere centred on New Zealand, using an orthographic projection.
Location of New Zealand, including outlying islands, its territorial claim in the Antarctic, and Tokelau
ISO 3166 codeNZ

New Zealand is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island (Te Ika-a-Māui) and the South Island (Te Waipounamu)—and over 700 smaller islands. It is the sixth-largest island country by area and lies east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland.

A developed country, it was the first to introduce a minimum wage, and the first to give women the right to vote. It ranks very highly in international measures of quality of life, human rights, and it has one of the lowest levels of perceived corruption in the world. It retains visible levels of inequality, having structural disparities between its Māori and European populations. New Zealand underwent major economic changes during the 1980s, which transformed it from a protectionist to a liberalised free-trade economy. The service sector dominates the national economy, followed by the industrial sector, and agriculture; international tourism is also a significant source of revenue. New Zealand is a member of the United Nations, Commonwealth of Nations, ANZUS, UKUSA, Five Eyes, OECD, ASEAN Plus Six, Asia-Pacific Economic Cooperation, the Pacific Community and the Pacific Islands Forum. It enjoys particularly close relations with the United States and is one of its major non-NATO allies; the United Kingdom; Samoa, Fiji, and Tonga; and with Australia, with a shared Trans-Tasman identity between the two countries stemming from centuries of British colonisation. (Full article...)

This is a Good article, an article that meets a core set of high editorial standards.

The Highlanders (Māori: Kahupeka; formerly the Otago Highlanders) is a New Zealand professional rugby union team based in Dunedin that compete in Super Rugby. The team was formed in 1996 to represent the lower South Island in the newly formed Super 12 competition, and includes the Otago, North Otago and Southland unions. The Highlanders take their name from the Scottish immigrants that founded the Otago, North Otago, and Southland regions in the 1840s and 1850s.

Their main ground through the 2011 Super Rugby season was Carisbrook in Dunedin, with home games occasionally being played in Invercargill and Queenstown. The Highlanders moved into Carisbrook's replacement, Forsyth Barr Stadium at University Plaza, for the 2012 season; the stadium opened in time for the 2011 Rugby World Cup, but after the Super Rugby season. (Full article...)

General images

The following are images from various New Zealand-related articles on Wikipedia.

More Did you know? - show different entries

...that megaherbs on the uninhabited New Zealand sub-antarctic islands almost became extinct by overbrowsing by livestock introduced to support shipwrecked sailors?

...that one of the Powelliphanta sp. is found only on a five hectare area northeast of Westport, New Zealand?

...that Mauisaurus was the largest plesiosaur to roam New Zealand waters and that it gets its name from the Māori demigod Māui?

...that it was during the Ngāti Whātua victory at the battle of Te Kai a te Karoro, or Seagull's Feast, that Ngā Puhi became the first Māori iwi to use muskets in combat?


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Damaged Catholic cathedral two months after the earthquake

A major earthquake occurred in Christchurch on Tuesday 22 February 2011 at 12:51 p.m. local time (23:51 UTC, 21 February). The Mw6.2 (ML6.3) earthquake struck the Canterbury region in the South Island, centred 6.7 kilometres (4.2 mi) south-east of the central business district. It caused widespread damage across Christchurch, killing 185 people in New Zealand's fifth-deadliest disaster. Scientists classified it as an intraplate earthquake and potentially an aftershock of the 2010 Canterbury earthquake.

Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the 2010 Canterbury earthquake and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was felt across the South Island and parts of the lower and central North Island. While the initial quake only lasted for approximately 10 seconds, the damage was severe because of the location and shallowness of the earthquake's focus in relation to Christchurch as well as previous quake damage. Subsequent population loss saw the Christchurch main urban area fall behind the Wellington equivalent, to decrease from second- to third-most populous area in New Zealand. Adjusted for inflation, the 2010–2011 Canterbury earthquakes caused over $44.8 billion in damages, making it New Zealand's costliest natural disaster and the 21st-most-expensive disaster in history. (Full article...)

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Looking out of one of the Cathedral Caves, in the Catlins, New Zealand.
Looking out of one of the Cathedral Caves, in the Catlins, New Zealand.

The Cathedral Caves is a large V shaped limestone sea cave located on Waipati Beach, 15 kilometres (9.3 mi) south of Papatowai, on the Catlins Coast in the southeast corner of New Zealand's South Island. The two main entrances join together within the cliff to form one big cave. One arm of the cave has a 30 metres (98 ft) high ceiling. Often blue penguins will emerge from the gloom at the far end of the cave. And occasionally a sealion might be around. (Full article...)

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