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New Zealand ( Māori: Aotearoa) is an island country located in the southwestern Pacific Ocean, near the centre of the water hemisphere. It consists of a large number of islands, estimated around 700, mainly remnants of a larger landmass now beneath the sea. The land masses by size are the South Island (or Te Waipounamu) and the North Island ...
Google Earth is a computer program that renders a 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposing satellite images, aerial photography, and GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and ...
[6] [7] In 1941, the Honorary Geographic Board of New Zealand renamed the hill to a 57-character name "Taumatawhakatangihangakoauauotamateapokaiwhenuakitanatahu", which has been an official name since 1948, and first appeared in a 1955 map. [8] The New Zealand Geographic Placenames Database, maintained by Land Information New ...
Find a globe in your local library or classroom and try this: Close the eyes, spin it and drop a finger randomly on its curved, glossy surface. In the age of Google Earth, watches that triangulate ...
Sketch of Dusky Sound in New Zealand 1773 and plan of the town and part of the settlement of New Plymouth 1850. 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 ...
Graph of New Zealand electricity generation capacity by year. This is a list of power stations in New Zealand. The list is not exhaustive – only power stations over 0.5 MW and significant power stations below 0.5 MW are listed. Power plants in New Zealand have different generating roles – for baseload, intermediate or peaking.
The Karikari Peninsula on the east coast of the far north of Northland, New Zealand, is between Rangaunu Harbour to the west, and Doubtless Bay to the southeast. It is a right-angled land mass of two relatively distinct parts. The rocky northern part, which has an east–west orientation and is approximately 17 km long, was originally an island ...
The Zealandia continent is largely made up of two nearly parallel ridges, separated by a failed rift, where the rift breakup of the continent stops and becomes a filled graben. The ridges rise above the sea floor to heights of 1,000–1,500 m (3,300–4,900 ft), with a few rocky islands rising above sea level. The ridges are continental rock ...