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Te Mata, Waikato District, Waikato
Te Mata is a small settlement from Hamilton and from Raglan. Demographics Te Mata is in an area which extends from Te Mata to Pakoka Landing and covers . The area is part of the larger Te Uku statistical area. Te Mata had a population of 174 in the 2023 New Zealand census, a decrease of 12 people (−6.5%) since the 2018 census, and an increase of 39 people (28.9%) since the 2013 census. There were 75 males and 96 females in 57 dwellings. 3.4% of people identified as LGBTIQ+. The median age was 37.8 years (compared with 38.1 years nationally). There were 42 people (24.1%) aged under 15 years, 27 (15.5%) aged 15 to 29, 81 (46.6%) aged 30 to 64, and 18 (10.3%) aged 65 or older. People could identify as more than one ethnicity. The results were 91.4% European (Pākehā), 22.4% Māori, 1.7% Asian, and 3.4% other, which includes people giving their ethnicity as "New Zealander". English was spoken by 100.0%, Māori language by 3.4%, and other languages by 6.9%. The percentag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand
New Zealand () is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and List of islands of New Zealand, over 600 smaller islands. It is the List of island countries, sixth-largest island country by area and lies east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The Geography of New Zealand, country's varied topography and sharp mountain peaks, including the Southern Alps (), owe much to tectonic uplift and volcanic eruptions. Capital of New Zealand, 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 subsequently developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European New Zealanders
New Zealanders of Ethnic groups in Europe, European descent are mostly of British people, British and Irish New Zealanders, Irish ancestry, with significantly smaller percentages of other European ancestries such as German New Zealanders, Germans, Polish New Zealanders, Poles, French New Zealanders, French, Dutch New Zealanders, Dutch, Croatian New Zealanders, Croats and other South Slavs, Greek New Zealanders, Greeks, and Scandinavian New Zealanders, Scandinavians. European New Zealanders are also known by the Māori-language loanword ''Pākehā''. Statistics New Zealand maintains the national classification standard for ethnicity. ''European'' is one of the six top-level ethnic groups, alongside Māori people, Māori, Pacific (Pasifika New Zealanders, Pasifika), Asian New Zealanders, Asian, Middle Eastern/Latin American/African (MELAA), and Other. Within the top-level European group are two second-level ethnic groups, ''New Zealand European'' and ''Other European''. New Zeal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron Oxide
An iron oxide is a chemical compound composed of iron and oxygen. Several iron oxides are recognized. Often they are non-stoichiometric. Ferric oxyhydroxides are a related class of compounds, perhaps the best known of which is rust. Iron oxides and oxyhydroxides are widespread in nature and play an important role in many geological and biological processes. They are used as iron ores, pigments, catalysts, and in thermite, and occur in hemoglobin. Iron oxides are inexpensive and durable pigments in paints, coatings and colored concretes. Colors commonly available are in the " earthy" end of the yellow/orange/red/brown/black range. When used as a food coloring, it has E number E172. Stoichiometries Iron oxides feature as ferrous ( Fe(II)) or ferric ( Fe(III)) or both. They adopt octahedral or tetrahedral coordination geometry. Only a few oxides are significant at the earth's surface, particularly wüstite, magnetite, and hematite. * Oxides of FeII ** FeO: ir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoria
Scoria or cinder is a pyroclastic, highly vesicular, dark-colored volcanic rock formed by ejection from a volcano as a molten blob and cooled in the air to form discrete grains called clasts.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. It is typically dark in color (brown, black or purplish-red), and basaltic or andesitic in composition. Scoria has relatively low density, as it is riddled with macroscopic ellipsoidal vesicles (gas bubbles), but in contrast to pumice, scoria always has a specific gravity greater than 1 and sinks in water. Scoria may form as part of a lava flow, typically near its surface, or as fragmental ejecta ( lapilli, blocks, and bombs), for instance in Strombolian eruptions that form steep-sided scoria cones, also called cinder cones. Scoria's holes or vesicles form when gases dissolved in the original magma come out of solution as it er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karioi
Karioi or Mount Karioi is a 2.4 million year old extinct stratovolcano SW of Raglan in the Waikato region of New Zealand's North Island. It was the earliest of the line of 6 calcalkalic volcanoes, the largest of which is Mount Pirongia (the others are at Kakepuku, Te Kawa, Tokanui, Waikeria and probably Puketotara). Karioi forms a background to many parts of Raglan. Karioi was also a Highway Board area around the maunga from 1870 to 1889, when it was absorbed (with Whaingaroa Board area and formed into Karioi Riding) into Raglan County Council. In 1876, it had a population of 112 in 27 houses and in 1889 119 ratepayers, 80 of them absentees. 19th century maps, documents and reports sometimes used the spelling Karehoe. Karioi is also a location on the Central Plateau (see article on Karioi railway station). History and culture Pre-European history Many iwi whakapapa back to Karioi, which features in several Māori legends. One says that, a long time ago, Karewa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Auckland Region
The Auckland region of New Zealand is built on a basement of greywacke rocks that form many of the islands in the Hauraki Gulf, the Hunua Ranges, and land south of Port Waikato. The Waitākere Ranges in the west are the remains of a large andesitic volcano, and Great Barrier Island was formed by the northern end of the Coromandel Volcanic Zone. The Auckland isthmus and North Shore, New Zealand, North Shore are composed of Waitemata sandstone and mudstone, and portions of the Northland Allochthon extend as far south as Albany, New Zealand, Albany. Little Barrier Island was formed by a relatively isolated andesitic volcano, active around 1 to 3 million years ago. The Manukau Harbour, Manukau and South Kaipara Harbours are protected by the recent sand dune deposits of the Āwhitu and South Kaipara Peninsulas. Recent basaltic volcanic activity has produced many volcanic cones throughout the Auckland region, including the iconic and youngest volcano Rangitoto Island. Basement rocks As ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Opotoru River
The Opotoru River is a river of the Waikato Region of New Zealand's North Island. It flows north, reaching the Raglan Harbour southwest of the town of Raglan, New Zealand, Raglan. There is no regular monitoring of pollution, but (31.2%) of the river has been fenced to protect it from farm stock. Name ThOct 1947 Lands and Survey one inch mapshows the name 'Opotoru R' applied to the tidal creek of the harbour and 'Opotoru S' to the stretch through Te Mata, Waikato District, Waikato, Te Mata. The 1971 2nd edition and current 1:50,000 maps (see http://www.topomap.co.nz/NZTopoMap/37544) show 'Opotoru River' for the lower part of the waterway, but 'Te Mata Stream' for the part up from the Te Hutewai Stream confluence. 'Te Mata Stream' appears to have been named 'Takapaunui Stream' in the 1910 postcards (see link below) and in the 1915 Bradbury's Illustrated Guide to The Raglan & Kawhia District. On 7 February 1974 the name Opotoru River was New Zealand Gazette, gazetted as the offi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irreligion In New Zealand
Irreligion in New Zealand refers to atheism, agnosticism, deism, religious scepticism and secular humanism in New Zealand society. Post-war New Zealand has become a highly secular country, meaning that religion does not play a major role in the lives of most people. Although New Zealand has no established religion, Christianity had been the most common religion since widespread European settlement in the 19th century. Demographics Statistics New Zealand gathers information on religious affiliation in the five-yearly census. Completing a census form is compulsory by law for every person in New Zealand on census night but respondents are able to object to answering the question of religious affiliation, and around 6% do object. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buddhism In New Zealand
Buddhism is New Zealand's third-largest religion after Christianity and Hinduism standing at 1.5% of the population of New Zealand. Buddhism originates in Asia and was introduced to New Zealand by immigrants from East Asia. History The first Buddhists in New Zealand were Chinese diggers in the Otago goldfields in the mid-1860s. Their numbers were small, and the 1926 census, the first to include Buddhism, recorded only 169. Buddhism grew significantly as a religion in New Zealand during the 1970s and 1980s with the arrival of Southeast Asian immigrants and refugees, coinciding with increased interest in Buddhist teaching from Western communities. Buddhist associations began forming, such as the Zen Society of New Zealand in 1972 (originally known as the Denkyo-ji Society), often fundraising to organise In the 1970s travel to Asian countries and visits by Buddhist teachers sparked an interest in the religious traditions of Asia, and significant numbers of New Zealanders adopte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Religious Beliefs
Māori or Maori can refer to: Relating to the Māori people * Māori people of New Zealand, or members of that group * Māori language, the language of the Māori people of New Zealand * Māori culture * Cook Islanders, the Māori people of the Cook Islands * Cook Islands Māori, the language of the Cook Islanders Ships * SS ''Maori'' (1893), a steamship of the Shaw Savill Line, shipwrecked 1909 * , a Royal Navy Tribal-class destroyer, sunk in 1915 * , a Royal Navy Tribal-class destroyer, launched 1936 and sunk 1942 * TEV ''Maori III'', a Union Steam Ship Company inter-island ferry, 1952–74 Sports teams * New Zealand Māori cricket team * New Zealand Māori rugby league team * New Zealand Māori rugby union team Other * ''Maori'', a 1988 novel by Alan Dean Foster * Mayotte Mayotte ( ; , ; , ; , ), officially the Department of Mayotte (), is an Overseas France, overseas Overseas departments and regions of France, department and region and single territorial collecti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christianity In New Zealand
Christianity in New Zealand dates to the arrival of missionary, missionaries from the Church Missionary Society who were welcomed onto the beach at Rangihoua Bay in December 1814. It soon became the predominant belief amongst the indigenous people, with over half of Māori people, Māori regularly attending church services within the first 30 years. Christianity remains New Zealand's largest religious group, but no one denomination is dominant and there is no official state church. According to the 2018 New Zealand census, 2018 census 38.17% of the population identified as Christians, Christian. The largest Christian groups are Anglican Church in New Zealand, Anglican, Catholic Church in New Zealand, Catholic and Presbyterian Church in New Zealand, Presbyterian. Christian organisations are the leading non-government providers of social services in New Zealand. History The first Christian church service, service conducted in New Zealand waters was probably to be carried out by F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
