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Te Miro
Te Miro is an area in the Waipa District of the Waikato Region of the North Island of New Zealand. Te Miro is situated 31 kilometres east southeast of Hamilton, New Zealand, Hamilton, and 24 kilometres northeast of Cambridge, New Zealand, Cambridge. Te Miro has a population of approximately 500. History The name Te Miro for the area first became used in 1916, when it was surveyed and developed for European settlement. Prior to that, the area was known as Maungakawa. The first Maori Pā settlement in the Te Miro area was by the Ngati Haua people at Te Kawehitiki (37 49 20; 175 34 50), located on the lower reaches of the Maungakawa volcanic cone, which is on the present day Hopehill farm,Hewitt, Joslyn (1995). ''Te Miro a history book to commemorate the 75th school and district reunion 1975''. Te Miro. at 789 Te Miro Road. There is a history of large Maori gatherings beginning at the site in the 1880s, with a notable large gathering in 1893. Maungakawa became a focal point for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dick Tonks
Richard William Tonks (born 21 February 1951) is a former national New Zealand rowing coach and a former rower who won a silver medal at the 1972 Summer Olympics in Munich. Through his coaching career he has coached crews to a total of 25 World Championship medals—including thirteen gold—and a total of seven Olympic medals—six of which were gold. Early life and rowing career Dick Tonks' father, Alan Tonks, was an accomplished rower and coach, and it is presumed that his influence was a major factor in Dick's taking up rowing at Wanganui Boys' College at the age of thirteen. He first competed at the Wanganui Secondary Schools Regatta in 1965 and subsequently—coached by his father—rowed in the school's first eight for three years. In 1970, back at the sport, he rowed for Otago in Dunedin and was able to earn a place on the national team in 1971. By 1972 he was stroking the New Zealand coxless four, alongside Ross Collinge, Dudley Storey and Noel Mills. The boat wen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wiremu Tamihana
Wiremu Tamihana Tarapipipi Te Waharoa ( – 27 December 1866), generally known as Wiremu Tamihana, was a leader of the Ngāti Hauā Māori iwi in nineteenth century New Zealand, and is sometimes known as the kingmaker for his role in the Māori King Movement. Early life Tarapipipi Te Waharoa, later known as Wiremu Tamihana, was born around 1805 at Tamahere on the Horotiu plains, the son of the Māori chief Te Waharoa and Rangi Te Wiwini. His father was the leader of the tribe Ngāti Hauā, which settled the area along the Waikato River near Horotiu as far east as the Kaimai Ranges. In his youth he fought in several expeditions that took place in the Taranaki and Waikato as part of the Musket Wars. In 1835, Tarapipipi met Reverend A. N. Brown, who had set up a Church Mission Society (CMS) station near the Matamata '' pā''. He was taught to read and write in the Māori language and soon would become a key communicator for his father. He was still from time to time engaged in outbre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato Institute Of Technology
The Waikato Institute of Technology, also known as Wintec, is an institute of technology based in New Zealand's Waikato region. Wintec offers over 130 degrees, diplomas and certificates. Wintec specialises in applied tertiary training for nurses, social workers, midwives, graphic designers, performing artists, engineers, trades people, early childhood teachers, horticulturists, arborists and sport scientists. Programmes range from Level 1 to Level 9. Wintec has 13,000 full and part-time students. Over 25% of Wintec students identify as Māori. History The institution was founded in 1924 as Hamilton Technical College. The name was changed to Waikato Technical Institute in 1968 and to The Waikato Polytechnic in 1987. The name changed again in 2001, to The Waikato Institute of Technology. On 1 April 2020, Waikato Institute of Technology was subsumed into New Zealand Institute of Skills & Technology alongside the 15 other Institutes of Technology and Polytechnics (ITPs). Locatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The University Of Waikato
, mottoeng = For The People , established = 1964; years ago , endowment = (31 December 2021) , budget = NZD $263.6 million (31 December 2020) , chancellor = Sir Anand Satyanand, GNZM, QSO, KStJ , vice_chancellor = Neil Quigley , city = Hamilton , province = Waikato , country = New Zealand (Māori: ''Kirikiriroa, Waikato, Aotearoa'') , administrative_staff = 1,499 (FTS, 2020) , students = 10,448 (EFTS, 2020) , type = Public research university , campus = Suburban 65 ha (160 acres) , colours = UW Red, Gold and Black , affiliations = ACU, ASAIHL, AACSB, AMBA, EQUIS , website Waikato.ac.nz, logo = The University of Waikato ( mi, Te Whare Wānanga o Waikato), is a public research university in Hamilton, New Zealand established in 1964. An additional campus is located in Tauranga. The university performs research in the disciplines of education, social sciences, and management and is an innovator in environmental science, marine and freshwater ecology, en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Education Review Office
The Education Review Office (ERO) (Māori: ''Te Tari Arotake Mātauranga'') is the public service department of New Zealand charged with reviewing and publicly reporting on the quality of education and care of students in all New Zealand schools and early childhood services. Led by a Chief Review Officer - the department's chief executive, the Office has approximately 150 designated review officers located in five regions. These regions are: Northern, Waikato/Bay of Plenty, Central, Southern, and Te Uepū ā-Motu (ERO's Māori review services unit). The Education Review Office, and the Ministry of Education are two separate public service departments. The functions and powers of the office are set out in Part 28 (sections 323–328) of the Education Act 1989. Reviews ERO reviews the education provided for school students in all state schools, private schools and kura kaupapa Māori Kura Kaupapa Māori are Māori-language immersion schools () in New Zealand where the ph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ministry Of Education (New Zealand)
The Ministry of Education (Māori: ''Te Tāhuhu o te Mātauranga'') is the public service department of New Zealand charged with overseeing the New Zealand education system. The Ministry was formed in 1989 when the former, all-encompassing Department of Education was broken up into six separate agencies. History The Ministry was established as a result of the Picot task force set up by the Labour government in July 1987 to review the New Zealand education system. The members were Brian Picot, a businessman, Peter Ramsay, an associate professor of education at the University of Waikato, Margaret Rosemergy, a senior lecturer at the Wellington College of Education, Whetumarama Wereta, a social researcher at the Department of Maori Affairs and Colin Wise, another businessman. The task force was assisted by staff from the Treasury and the State Services Commission (SSC), who may have applied pressure on the task force to move towards eventually privatizing education, as had ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Miro School
Te Miro is an area in the Waipa District of the Waikato Region of the North Island of New Zealand. Te Miro is situated 31 kilometres east southeast of Hamilton, and 24 kilometres northeast of Cambridge. Te Miro has a population of approximately 500. History The name Te Miro for the area first became used in 1916, when it was surveyed and developed for European settlement. Prior to that, the area was known as Maungakawa. The first Maori Pā settlement in the Te Miro area was by the Ngati Haua people at Te Kawehitiki (37 49 20; 175 34 50), located on the lower reaches of the Maungakawa volcanic cone, which is on the present day Hopehill farm,Hewitt, Joslyn (1995). ''Te Miro a history book to commemorate the 75th school and district reunion 1975''. Te Miro. at 789 Te Miro Road. There is a history of large Maori gatherings beginning at the site in the 1880s, with a notable large gathering in 1893. Maungakawa became a focal point for the Waikato King movement led by King Tawhiao. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ignimbrite
Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ''ignimbrite'' from the Latin ''igni-'' [fire] and ''imbri-'' [rain]. Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when Lithification, lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli-tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of New Zealand
New Zealand is divided into sixteen regions () for local government in New Zealand, local government purposes. Eleven are administered by regional councils (the top tier of local government), and five are administered by Unitary authority#New Zealand, unitary authorities, which are territorial authorities of New Zealand, territorial authorities (the second tier of local government) that also perform the functions of regional councils. The Chatham Islands#Government, Chatham Islands Council is not a region but is similar to a unitary authority, authorised under its own legislation. Current regions History and statutory basis The regional councils are listed in Part 1 of Schedule 2 of the Local Government Act 2002 (New Zealand), Local Government Act 2002, along with reference to the ''New Zealand Gazette, Gazette'' notices that established them in 1989. The Act requires regional councils to promote sustainable developmentthe social, economic, environmental and cultural well-bei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
