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An annotated relief map. New Zealand is located in the South Pacific Ocean at , near the centre of the water hemisphere. [4] It is a long and narrow country, extending 1,600 kilometres (990 mi) along its north-north-east axis with a maximum width of 400 kilometres (250 mi). [5]
A true-colour image of the South Island, after a powerful winter storm swept across New Zealand on 12 June 2006 Lake Ōhau Aoraki / Mount Cook is the tallest mountain in New Zealand. The South Island, with an area of 150,437 km 2 (58,084 sq mi), [1] is the largest landmass of New Zealand; it contains about one-quarter of the New Zealand ...
The Southern Ocean then extended from Antarctica northwards to latitude 40° south between Cape Agulhas in Africa (long. 20° east) and Cape Leeuwin in Western Australia (long. 115° east), and extended to latitude 55° south between Auckland Island of New Zealand (long. 165° or 166° east) and Cape Horn in South America (long. 67° west). [16]
The location of New Zealand on a globe. The following outline is provided as an overview of and topical guide to New Zealand: . New Zealand is an island country located in the western South Pacific Ocean comprising two large islands, the North Island and the South Island, and numerous smaller islands, most notably Stewart Island / Rakiura and the Chatham Islands. [1]
Water in the Southern Ocean south of, for example, New Zealand, resembles the water in the Southern Ocean south of South America more closely than it resembles the water in the Pacific Ocean. The Southern Ocean has typical depths of between 4,000 and 5,000 m (13,000 and 16,000 ft) over most of its extent with only limited areas of shallow water ...
The South Island [a] (Māori: Te Waipounamu [tɛ wɐ.i.pɔ.ʉ.nɐ.mʉ], lit. 'the waters of Greenstone') is the largest of the three major islands of New Zealand in surface area, the others being the smaller but more populous North Island and sparsely populated Stewart Island.
New Zealand [a] 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 600 smaller islands.
The convergent plate boundary that runs northwards from New Zealand's North Island is called the Kermadec-Tonga subduction zone. This subduction zone is associated with the volcanism that gave rise to the Kermadec and Tongan islands. There is a transform fault that currently traverses New Zealand's South Island, known as the Alpine Fault.