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Te Kawa
Te Kawa is a rural community in the Ōtorohanga District and Waikato region of New Zealand's North Island. It lies just to the south of the volcanic hills of Kakepuku and Te Kawa. Until the swamp was drained in the 1900s, Te Kawa was well known for its eels. Te Kawa railway station, a station on the North Island Main Trunk, was located in the area. It operated from 9 March 1887 and closed 17 October 1971. A post office was open by 1909 and a dairy factory and a school existed in 1913. Te Kawa Bridge over the Waipā opened in 1915. A town hall opened in 1928. Te Whakaaro Kotahi Marae in Te Kawa is a meeting ground of the Ngāti Maniapoto hapū of Te Kanawa. It includes a small building. Demographics Te Kawa settlement is in three SA1 statistical areas which cover . The SA1 areas are part of the larger Te Kawa statistical area. The SA1 areas had a population of 504 at the 2018 New Zealand census, an increase of 84 people (20.0%) since the 2013 census, and an increase of ...
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Te Kawa Railway Station
Te Kawa railway station was a station on the North Island Main Trunk in New Zealand, located at Te Kawa. The railway crossed (or 8,000) Te Kawa Swamp to the north of the station on a embankment. Culverts were included to maintain the effectiveness of eel weirs in the swamp and provide for the flow of water. A post office was open by 1909 and a drainage board set up, which was extended in 1915, by which time the station was handling traffic for Waikeria Prison. In 1908 the station was being considered as a junction for a line to Kawhia and Raglan and by 1920 as a junction on a railway from Kawhia to Rotorua. On 14 September 1913 the name of the station was changed from Kawa to Te Kawa. In 1917 a telephone was reported as connected, though another report put the date as 1929. By 1980 there was a passing loop A passing loop (UK usage) or passing siding (North America) (also called a crossing loop, crossing place, refuge loop or, colloquially, a hole) is a place on a sing ...
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Waikato Region
Waikato () is a local government region of the upper North Island of New Zealand. It covers the Waikato District, Waipa District, Matamata-Piako District, South Waikato District and Hamilton City, as well as Hauraki, Coromandel Peninsula, the northern King Country, much of the Taupō District, and parts of Rotorua District. It is governed by the Waikato Regional Council. The region stretches from Coromandel Peninsula in the north, to the north-eastern slopes of Mount Ruapehu in the south, and spans the North Island from the west coast, through the Waikato and Hauraki to Coromandel Peninsula on the east coast. Broadly, the extent of the region is the Waikato River catchment. Other major catchments are those of the Waihou, Piako, Awakino and Mokau rivers. The region is bounded by Auckland on the north, Bay of Plenty on the east, Hawke's Bay on the south-east, and Manawatū-Whanganui and Taranaki on the south. Waikato Region is the fourth largest region in the country in a ...
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2018 New Zealand Census
Eighteen or 18 may refer to: * 18 (number), the natural number following 17 and preceding 19 * one of the years 18 BC, AD 18, 1918, 2018 Film, television and entertainment * ''18'' (film), a 1993 Taiwanese experimental film based on the short story ''God's Dice'' * ''Eighteen'' (film), a 2005 Canadian dramatic feature film * 18 (British Board of Film Classification), a film rating in the United Kingdom, also used in Ireland by the Irish Film Classification Office * 18 (''Dragon Ball''), a character in the ''Dragon Ball'' franchise * "Eighteen", a 2006 episode of the animated television series ''12 oz. Mouse'' Music Albums * ''18'' (Moby album), 2002 * ''18'' (Nana Kitade album), 2005 * '' 18...'', 2009 debut album by G.E.M. Songs * "18" (5 Seconds of Summer song), from their 2014 eponymous debut album * "18" (One Direction song), from their 2014 studio album ''Four'' * "18", by Anarbor from their 2013 studio album '' Burnout'' * "I'm Eighteen", by Alice Cooper commo ...
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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. 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 was the husband of Karioi, but he flirted with her sister, Pirongia, and was cast into ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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Volcanology Of New Zealand
The volcanism of New Zealand has been responsible for many of the country's geographical features, especially in the North Island and the country's outlying islands. While the land's volcanism dates back to before the Zealandia microcontinent rifted away from Gondwana 60–130 million years ago, activity continues today with minor eruptions occurring every few years. This recent activity is primarily due to the country's position on the boundary between the Indo-Australian and Pacific Plates, a part of the Pacific Ring of Fire, and particularly the subduction of the Pacific Plate under the Indo-Australian Plate. New Zealand's rocks record examples of almost every kind of volcanism observed on Earth, including some of the world's largest eruptions in geologically recent times. None of the South Island's volcanoes are active. Major eruptions New Zealand has been the site of many large explosive eruptions during the last two million years, including several of supervolcano ...
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Islam In New Zealand
Islam in New Zealand is a religious affiliation representing about 1.3% of the total population. Small numbers of Muslim immigrants from South Asia and eastern Europe settled in New Zealand from the early 1900s until the 1960s. Large-scale Muslim immigration began in the 1970s with the arrival of Fiji Indians, followed in the 1990s by refugees from various war-torn countries. The first Islamic centre in New Zealand opened in 1959 and there are now several mosques and two Islamic schools. The majority of Muslims in New Zealand are Sunni, with significant Shia and Ahmadiyya minorities. The Ahmadiyya Community has translated the Qur'an into the Māori language. History Early migration, 19th century The earliest Muslim presence in New Zealand dates back to the late 19th century. The first Muslims in New Zealand were an Indian family who settled in Cashmere, Christchurch, in the 1850s. The 1874 government census reported 15 Chinese Muslim gold diggers working in the Dunstan gold ...
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Māori Religion
Māori religion encompasses the various religious beliefs and practices of the Māori, the Polynesian indigenous people of New Zealand. Traditional Māori religion Traditional Māori religion, that is, the pre-European belief-system of the Māori, differed little from that of their tropical Eastern Polynesian homeland ( Hawaiki Nui), conceiving of everything - including natural elements and all living things - as connected by common descent through whakapapa or genealogy. Accordingly, Māori regarded all things as possessing a life force or mauri. Illustrating this concept of connectedness through genealogy are the major personifications dating from before the period of European contact: * Tangaroa was the personification of the ocean and the ancestor or origin of all fish. * Tāne was the personification of the forest and the origin of all birds. * Rongo was the personification of peaceful activities and agriculture and the ancestor of cultivated plants. (Some sources ref ...
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Christianity In New Zealand
Christianity in New Zealand dates to the arrival of 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 an estimated 60% of Māori pledging allegiance to the Christian message within the first 35 years. It remains New Zealand's largest religious group despite there being no official state church. Today, slightly less than half the population identify as Christian. The largest Christian groups are Catholic, Anglican and Presbyterian. Christian organisations are the leading non-government providers of social services in New Zealand. History The first Christian services conducted in New Zealand were carried out by Father Paul-Antoine Léonard de Villefeix, the Dominican chaplain on the ship ''Saint Jean Baptiste'' commanded by the French navigator and explorer Jean-François-Marie de Surville. Villefeix was the first Christian minister to set ...
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Asian New Zealanders
Asian New Zealanders are New Zealanders of Asian ancestry (including naturalised New Zealanders who are immigrants from specific regions in Asia and descendants of such immigrants). Terminology In the New Zealand census, the term refers to a pan-ethnic group that includes diverse populations who have ancestral origins in East Asia (e.g. Chinese New Zealanders, Korean New Zealanders, Japanese New Zealanders), Southeast Asia (e.g. Filipino New Zealanders, Vietnamese New Zealanders, Malaysian New Zealanders), and South Asia (e.g. Nepalese New Zealanders, Indian New Zealanders, Sri Lankan New Zealanders, Bangladeshi New Zealanders, Pakistani New Zealanders). Notably, New Zealanders of West Asian and Central Asian ancestry are excluded from this term. Colloquial usage of ''Asian'' in New Zealand excludes Indians and other peoples of South Asian descent. ''Asian'' as used by Statistics New Zealand includes South Asian ethnic group. The first Asians in New Zealand were Chinese wo ...
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Pasifika New Zealanders
Pasifika New Zealanders are a pan-ethnic group of New Zealanders associated with, and descended from, the indigenous peoples of the Pacific Islands outside of New Zealand itself (also known as Pacific Islanders). They form the fourth-largest ethnic grouping in the country, after European-descended Pākehā, indigenous Māori, and Asian New Zealanders. There are over 380,000 Pasifika people in New Zealand, with the majority living in Auckland. 8% of the population of New Zealand identifies as being of Pacific origin. History Prior to the Second World War Pasifika in New Zealand numbered only a few hundred. Wide-scale Pasifika migration to New Zealand began in the 1950s and 1960s, typically from countries associated with the Commonwealth and the Realm of New Zealand, including Western Samoa (modern-day Samoa), the Cook Islands and Niue. In the 1970s, governments (both Labour and National), migration officials, and special police squads targeted Pasifika illegal overstayers. Paci ...
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