Great Mercury Island
The Mercury Islands are a group of seven islands off the northeast coast of New Zealand's North Island. They are located off the coast of the Coromandel Peninsula, and northeast of the town of Whitianga. History The Ngāti Karaua (a hapu of the Ngāti Whanaunga) and the Ngāti Hei inhabited the islands since the 14th century. A settler claimed to have bought Great Mercury Island in 1839.https://www.govt.nz/assets/Documents/OTS/Ngati-Hei/Ngati-Hei-Deed-of-Settlement-17-Aug-2017.pdf Great Mercury (Ahuahu), Kawhitu or Stanley Island and Double Island (Moturehu) where purchased and taken as crown land in 1858–65. These included Whakakapua (73 acres) and Kowhaka (21 acres) being purchased in January 1865. Despite inhabiting Ahuahu, the Ngati Hei were not consulted about this purchase. A 2017 settlement recognized the Ngāti Hei as having a legitimate claim to Great Mercury Island. Description The main chain of the Mercury Islands consists of the large Great Mercury Island (al ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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South Pacific Ocean
South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz'' ("south"), possibly related to the same Proto-Indo-European root that the word ''sun'' derived from. Some languages describe south in the same way, from the fact that it is the direction of the sun at noon (in the Northern Hemisphere), like Latin meridies 'noon, south' (from medius 'middle' + dies 'day', cf English meridional), while others describe south as the right-hand side of the rising sun, like Biblical Hebrew תֵּימָן teiman 'south' from יָמִין yamin 'right', Aramaic תַּימנַא taymna from יָמִין yamin 'right' and Syriac ܬܰܝܡܢܳܐ taymna from ܝܰܡܝܺܢܳܐ yamina (hence the name of Yemen, the land to the south/right of the Levant). Navigation By convention, the ''bottom or down-facing side'' of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Last Glacial Maximum
The Last Glacial Maximum (LGM), also referred to as the Late Glacial Maximum, was the most recent time during the Last Glacial Period that ice sheets were at their greatest extent. Ice sheets covered much of Northern North America, Northern Europe, and Asia and profoundly affected Earth's climate by causing drought, desertification, and a large drop in sea levels. Based on changes in position of ice sheet margins dated via terrestrial cosmogenic nuclides and radiocarbon dating, growth of ice sheets commenced 33,000 years ago and maximum coverage was between 26,500 years and 19–20,000 years ago, when deglaciation commenced in the Northern Hemisphere, causing an abrupt rise in sea level. Decline of the West Antarctica ice sheet occurred between 14,000 and 15,000 years ago, consistent with evidence for another abrupt rise in the sea level about 14,500 years ago. Glacier fluctuations around the Strait of Magellan suggest the peak in glacial surface area was constrained to betwee ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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The Edge
David Howell Evans (born 8 August 1961), better known as the Edge or simply Edge,McCormick (2006), pp. 21, 23–24 is an English-born Irish musician, singer, and songwriter. He is best known as the lead guitarist, keyboardist, and backing vocalist of the rock band U2. A member of the group since its inception, he has recorded 14 studio albums with them as well as one solo record. His understated style of guitar playing, a signature of U2's music, is distinguished by chiming timbres, use of rhythmic delay, drone notes, harmonics, and an extensive use of effects units. Born in England to Welsh parents and raised in Ireland, the Edge formed the band that would become U2 with his classmates at Mount Temple Comprehensive School and his elder brother Dik in 1976. Inspired by the ethos of punk rock and its basic arrangements, the group began to write its own material. They eventually became one of the most successful acts in popular music, with albums such as 1987's ''The Joshua Tr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bono
Paul David Hewson (born 10 May 1960), known by his stage name Bono (), is an Irish singer-songwriter, activist, and philanthropist. He is the lead vocalist and primary lyricist of the rock band U2. Born and raised in Dublin, he attended Mount Temple Comprehensive School where in 1976 he began dating his future wife, Alison Stewart, as well as forming, with schoolmates, the band that became U2. Bono soon established himself as a passionate frontman for the band through his expressive vocal style and grandiose gestures and songwriting. His lyrics frequently include social and political themes, and religious imagery inspired by his Christian beliefs. During U2's early years, Bono's lyrics contributed to the group's rebellious and spiritual tone. As the band matured, his lyrics became inspired more by personal experiences shared with the other members. As a member of U2, Bono has received 22 Grammy Awards and has been inducted into the Rock and Roll Hall of Fame. Aside fro ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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New Zealand Dollar
The New Zealand dollar ( mi, tāra o Aotearoa; sign: $, NZ$; code: NZD) is the official currency and legal tender of New Zealand, the Cook Islands, Niue, the Ross Dependency, Tokelau, and a British territory, the Pitcairn Islands. Within New Zealand, it is almost always abbreviated with the dollar sign ($). "$NZ" or "NZ$" are sometimes used when necessary to distinguish it from other dollar-denominated currencies. Introduced in 1967, the dollar is subdivided into 100 cents. Altogether it has five coins and five banknotes with the smallest being the 10-cent coin; smaller denominations have been discontinued due to inflation and production costs. In the context of currency trading, the New Zealand dollar is sometimes informally called the "Kiwi" or "Kiwi dollar", since the flightless bird, the Kiwi (bird), kiwi, is depicted on its New Zealand one-dollar coin, one-dollar coin. It is the tenth most traded currency in the world, representing 2.1% of global foreign exchange marke ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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David Richwhite
David MacKellar Richwhite (born 1948) is a New Zealand investment banker and was a partner in Fay, Richwhite & Company with Sir Michael Fay. Educated at King's College, Auckland and the University of Otago, where he graduated in 1974 with a Bachelor of Commerce degree, Richwhite's personal wealth was largely acquired during the late 1980s and early 1990s. During this period he had a significant and controversial role in the structural adjustment of the New Zealand economy undertaken by the Fourth Labour Government. Fay, Richwhite & Company was the prime focus of the "Winebox Inquiry" which dealt with, among other things, tax-avoidance arrangements in the Cook Islands. The publicity surrounding the inquiry generated considerable public ill-feeling towards Fay and Richwhite. Based in Geneva from 1998 to 2003, Richwhite now lives with his family in London. Fay Richwhite David Richwhite and Sir Michael Fay formed Fay Richwhite in 1973 which grew to become one of the leading merc ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Michael Fay (banker)
Sir Humphrey Michael Gerard Fay (born 10 April 1949) is a New Zealand merchant banker and partner in the merchant bank Fay Richwhite. He is one of the ten richest men in New Zealand. His personal wealth was largely acquired during the late 1980s and early 1990s, which included the period in which he had a significant role in the structural adjustment of the New Zealand economy undertaken by New Zealand's Fourth Labour Government. He is thought to be worth in excess of NZD 920 million, making him the 10th richest New Zealand citizen in 2017. Early life and family Fay was born in Auckland on 10 April 1949. He was educated at St Peter's College, Auckland and St Patrick's College, Silverstream, and studied law at Victoria University of Wellington, graduating LLB in 1971. In 1983, he married Sarah Ann Williams, and the couple went on to have three children. Fay Richwhite Michael Fay and David Richwhite are best known for gaining wealth in a series of loosely regulated privatisation ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kauri Gum
Kauri gum is resin from kauri trees (''Agathis australis''), which historically had several important industrial uses. It can also be used to make crafts such as jewellery. Kauri forests once covered much of the North Island of New Zealand, before the arrival of people caused deforestation, causing several areas to revert to sand dunes, scrubs, and swamps. Even afterwards, ancient kauri fields continued to provide a source for the gum and the remaining forests.Hayward, pp 4–5 Kauri gum forms when resin from kauri trees leaks out through fractures or cracks in the bark, hardening with the exposure to air. Lumps commonly fall to the ground and can be covered with soil and forest litter, eventually fossilising. Other lumps form as branches forked or trees are damaged, releasing the resin.Hayward, p 2 Uses The Māori had many uses for the gum, which they called ''kapia''. Fresh gum was used as a type of chewing gum (older gum was softened by soaking and mixing with juice of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Auckland War Memorial Museum
The Auckland War Memorial Museum Tāmaki Paenga Hira (or simply the Auckland Museum) is one of New Zealand's most important museums and war memorials. Its collections concentrate on New Zealand history (and especially the history of the Auckland Region), natural history, and military history. The present museum building was constructed in the 1920s in the neo-classicist style, and sits on a grassed plinth (the remains of a dormant volcano) in the Auckland Domain, a large public park close to the Auckland CBD. Auckland Museum's collections and exhibits began in 1852. In 1867 Aucklanders formed a learned society – the Auckland Philosophical Society, later the Auckland Institute. Within a few years the society merged with the museum and '' Auckland Institute and Museum'' was the organisation's name until 1996. Auckland War Memorial Museum was the name of the new building opened in 1929, but since 1996 was more commonly used for the institution as well. From 1991 to 2003 the muse ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Colony Of New Zealand
The Colony of New Zealand was a Crown colony of the United Kingdom of Great Britain and Ireland that encompassed the islands of New Zealand from 1841 to 1907. The power of the British government was vested in the Governor of New Zealand, as the representative of their monarch. The colony had three capitals: Old Russell in 1841; Auckland from 1841 to 1865; and Wellington, which was the capital until the colony's reorganisation into a Dominion, and continues to be the capital of New Zealand till the present day. In 1852, the colony was granted self-government with the passage of the New Zealand Constitution Act 1852. Subsequently, the first parliament was elected in 1853, and responsible government was established in 1856. In 1907, the colony became the Dominion of New Zealand, which heralded a more explicit recognition of self-government within the British Empire. History Establishment Following a proclamation of sovereignty over New Zealand from Sydney in January ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent to granite. Rhyolitic magma is extremely viscous, due to its high silica content. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been extensively used for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil amendment. Description Rhyolite i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |