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The southernmost settlement in New Zealand is Oban, on Stewart Island, although there is a meteorological station on Campbell Island, though this is no longer permanently staffed since 1995. The southernmost town in New Zealand with a population over 1000 is Bluff. New Zealand's southernmost city is Invercargill - also its westernmost city.
New Zealand is the sixth-largest island country in the world, with a land size of 268,680 km 2 (103,740 sq mi). [3] New Zealand's landscapes range from the fiord-like sounds of the southwest to the sandy beaches of the subtropical Far North.
Aoraki / Mount Cook is the highest point in New Zealand, at 3,724 metres. The South Island is the largest landmass of New Zealand. It is divided along its length by the Southern Alps. [97] 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). [98]
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 South Island (Māori: Te Waipounamu [tɛ wɐ.i.pɔ.ʉ.nɐ.mʉ], lit. 'the waters of Greenstone', officially South Island or Te Waipounamu or archaically New Munster) 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.
The summit was first reached probably by Sir Edmund Hillary of New Zealand and Tenzing Norgay Sherpa of Nepal in 1953. The point farthest from Earth's centre is the summit of Chimborazo [11] in Ecuador, at 6,384.4 km (3,967.1 mi) from Earth's centre; the peak's elevation relative to sea level is 6,263.47 m (20,549 ft).
The geology of New Zealand is noted for its volcanic activity, earthquakes and geothermal areas because of its position on the boundary of the Australian Plate and Pacific Plates. New Zealand is part of Zealandia , a microcontinent nearly half the size of Australia that broke away from the Gondwanan supercontinent about 83 million years ago. [ 1 ]
The cartography of New Zealand is the history of surveying and creation of maps of New Zealand. Surveying in New Zealand began with the arrival of Abel Tasman in the mid 17th century. [ 1 ] Cartography and surveying have developed in incremental steps since that time till the integration of New Zealand into a global system based on GPS and the ...