Pukaki (chief)
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Pukaki (chief)
Pukaki was an 18th-century chief of the Te Arawa, Arawa iwi of New Zealand. His portrait appears on the New Zealand 20 cent coin minted from 1990 to 2008. The name has been used for several New Zealand items: *Pukaki, one of the volcanic cones of the Auckland volcanic field *Lake Pukaki, a lake in Canterbury, New Zealand *Pukaki River, a river in Canterbury *''HMNZS Pukaki'', the name used by three ships of the Royal New Zealand Navy {{disambiguation ...
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Te Arawa
Te Arawa is a confederation of Māori iwi and hapu (tribes and sub-tribes) of New Zealand who trace their ancestry to the Arawa migration canoe (''waka'')."Te Arawa"
''Te Ara – the Encyclopedia of New Zealand''.
The tribes are based in the and areas and have a population of around 40,000.


History

The history of the Te Arawa people is inextricably linked to the Arawa canoe. The Te Arawa tribes have a close historical interest in the lakes around Rotorua. Many Te Arawa men fought for the Colonial Government in the

New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about 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. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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New Zealand 20 Cent Coin
The New Zealand twenty-cent coin is the second-lowest-denomination coin of the New Zealand dollar. The 20-cent coin was introduced when the New Zealand dollar was introduced on 10 July 1967, replacing the New Zealand florin coin. Its original reverse of a kiwi was changed in 1990 when the image was moved onto the one-dollar coin. In 2006 its size was reduced and its edge altered to a Spanish flower as part of a revision of New Zealand's coins, which also saw its alloy become nickel-plated steel instead of cupro-nickel. Design 1967 to 1990 On 10 July 1967, New Zealand decimalised its currency, replacing the pound with the dollar at a rate of one pound to two dollars and one shilling to ten cents. The 20-cent coin directly replaced the one-florin coin, which had been worth two shillings. Like the florin, the new 20-cent coin was made of cupronickel, 28.58 mm in diameter, 11.31 grams in weight, and had 100% edge milling. The 20-cent coin retained the presence of a ki ...
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Auckland Volcanic Field
The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately 53 volcanoes in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupō.Ian E.M. Smith and Sharon R. Allen. Auckland volcanic field geology'. Volcanic Hazards Working Group, Civil Defence Scientific Advisory Committee. Retrieved 30 March 2013. Also ...
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Lake Pukaki
Lake Pukaki is the largest of three roughly parallel alpine lakes running north–south along the northern edge of the Mackenzie Basin on New Zealand's South Island. The others are Lakes Tekapo and Ohau. All three lakes were formed when the terminal moraines of receding glaciers blocked their respective valleys, forming moraine-dammed lakes. The Alps2Ocean mountain bike trail follows the edge of Lake Pukaki for part of its length. Geography The glacial feed to the lakes gives them a distinctive blue colour, created by glacial flour, the extremely finely ground rock particles from the glaciers. Lake Pukaki covers an area of 178.7 km², and the surface elevation of the lake normally ranges from 518.2 to 532 metres above sea level. The lake is fed at its northern end by the braided Tasman River, which has its source in the Tasman and Hooker Glaciers, close to Aoraki / Mount Cook. To the west of Lake Pukaki lies the Ben Ohau mountain range with Ben Dhu (1607m) and Betty ...
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Pukaki River
The Pukaki River flows through the Mackenzie Basin, Canterbury, in New Zealand's South Island. Originally, the river flowed southwest for from the southern end of Lake Pukaki before joining with the Tekapo River and flowing into the northern end of Lake Benmore. However, all water from Lake Pukaki is now diverted into a canal which is fed through three hydroelectric stations before being returned directly into Lake Benmore, as part of the Waitaki Hydroelectric scheme. Occasionally, water may be spilled down the riverbed when Lake Pukaki reaches its maximum height, or if a canal or power station requires servicing. In 2010, Meridian Energy Meridian Energy Limited is a New Zealand electricity generator and retailer. The company generates the largest proportion of New Zealand's electricity, generating 35 percent of the country's electricity in the year ending December 2014, and is ... applied for resource consents to build a 35 MW power station at Pukaki's gate 18. Consent w ...
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