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The early European settlers divided New Zealand into provinces, which had a degree of autonomy.[125] Because of financial pressures and the desire to consolidate railways, education, land sales and other policies, government was centralised and the provinces were abolished in 1876.[126] The provinces are remembered in regional public holidays[127] and sporting rivalries.[128] Since 1876, various councils have administered local areas under legislation determined by the central government.[125][129] In 1989, the government reorganised local government into the current two-tier structure of regional councils and territorial authorities.[130] The 249 municipalities[130] that existed in 1975 have now been consolidated into 67 territorial authorities and 11 regional councils.[131] The regional councils' role is to regulate "the natural environment with particular emphasis on resource management",[130] while territorial authorities are responsible for sewage, water, local roads, building consents and other local matters.[132][133] Five of the territorial councils are unitary authorities and also act as regional councils.[133] The territorial authorities consist of 13 city councils, 53 district councils, and the Chatham Islands Council. While officially the Chatham Islands Council is not a unitary authority, it undertakes many functions of a regional council.[134]
The Realm of New Zealand, one of 16 Commonwealth realms,[135] is the entire area over which the queen of New Zealand is sovereign, and comprises New Zealand, Tokelau, the Ross Dependency, the Cook Islands and Niue.[68] The Cook Islands and Niue are self-governing states in free association with New Zealand.[136][137] The New Zealand Parliament cannot pass legislation for these countries, but with their consent can act on behalf of them in foreign affairs and defence. Tokelau is classified as a non-self-governing territory, but is administered by a council of three elders (one from each Tokelauan atoll).[138] The Ross Dependency is New Zealand's territorial claim in Antarctica, where it operates the Scott Base research facility.[139] New Zealand nationality law treats all parts of the realm equally, so most people born in New Zealand, the Cook Islands, Niue, Tokelau and the Ross Dependency are New Zealand citizens

New Zealand is located near the centre of the water hemisphere and is made up of two main islands and a number of smaller islands. The two main islands (the North Island, or Te Ika-a-Maui, and the South Island, or Te Waipounamu) are separated by Cook Strait, 22 kilometres (14 mi) wide at its narrowest point.[142] Besides the North and South Islands, the five largest inhabited islands are Stewart Island (across the Foveaux Strait), Chatham Island, Great Barrier Island (in the Hauraki Gulf),[143] D'Urville Island (in the Marlborough Sounds)[144] and Waiheke Island (about 22 km (14 mi) from central Auckland).[145] A large mountain with a lake in the foreground Aoraki / Mount Cook is the highest point of New Zealand, at 3,724 metres. Snow-capped mountain range The Southern Alps stretch for 500 kilometres down the South Island. New Zealand is long and narrow—over 1,600 kilometres (990 mi) along its north-north-east axis with a maximum width of 400 kilometres (250 mi)[146]—with about 15,000 km (9,300 mi) of coastline[147] and a total land area of 268,000 square kilometres (103,500 sq mi).[148] Because of its far-flung outlying islands and long coastline, the country has extensive marine resources. Its exclusive economic zone is one of the largest in the world, covering more than 15 times its land area.[149] The South Island is the largest landmass of New Zealand. It is divided along its length by the Southern Alps.[150] There are 18 peaks over 3,000 metres (9,800 ft), the highest of which is Aoraki / Mount Cook at 3,724 metres (12,218 ft).[151] Fiordland's steep mountains and deep fiords record the extensive ice age glaciation of this southwestern corner of the South Island.[152] The North Island is less mountainous but is marked by volcanism.[153] The highly active Taupo Volcanic Zone has formed a large volcanic plateau, punctuated by the North Island's highest mountain, Mount Ruapehu (2,797 metres (9,177 ft)). The plateau also hosts the country's largest lake, Lake Taupo,[154] nestled in the caldera of one of the world's most active supervolcanoes.[155] The country owes its varied topography, and perhaps even its emergence above the waves, to the dynamic boundary it straddles between the Pacific and Indo-Australian Plates.[156] New Zealand is part of Zealandia, a microcontinent nearly half the size of Australia that gradually submerged after breaking away from the Gondwanan supercontinent.[157][158] About 25 million years ago, a shift in plate tectonic movements began to contort and crumple the region. This is now most evident in the Southern Alps, formed by compression of the crust beside the Alpine Fault. Elsewhere the plate boundary involves the subduction of one plate under the other, producing the Puysegur Trench to the south, the Hikurangi Trench east of the North Island, and the Kermadec and Tonga Trenches[159] further north.[156] New Zealand is part of a region known as Australasia, together with Australia.[160] It also forms the southwestern extremity of the geographic and ethnographic region called Polynesia.[161] The term Oceania is often used to denote the wider region encompassing the Australian continent, New Zealand and various islands in the Pacific Ocean that are not included in the seven-continent model.[162] Landscapes of New Zealand Rural scene near Queenstown The Emerald Lakes, Mt Tongariro Lake Gunn Pencarrow Head, Wellington Climate Main article: Climate of New Zealand New Zealand's climate is predominantly temperate maritime (Köppen: Cfb), with mean annual temperatures ranging from 10 °C (50 °F) in the south to 16 °C (61 °F) in the north.[163] Historical maxima and minima are 42.4 °C (108.32 °F) in Rangiora, Canterbury and -25.6 °C (-14.08 °F) in Ranfurly, Otago.[164] Conditions vary sharply across regions from extremely wet on the West Coast of the South Island to almost semi-arid in Central Otago and the Mackenzie Basin of inland Canterbury, and subtropical in Northland.[165][166] Of the seven largest cities, Christchurch is the driest, receiving on average only 640 millimetres (25 in) of rain per year

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