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Hinuera Gap
Hinuera is a settlement in the Waikato Region of New Zealand's North Island. It is located along State Highway 29, approximately halfway between the cities of Hamilton and Tauranga. It also contains the Hinuera cliffs along State Highway 29. Hinuera had a butter factory from 1922 to 1987. Electric street lights were introduced in 1923. Geography Hinuera Stone, or Ongatiti Ignimbrite, is a Late Pleistocene, light-brown rock containing angular fragments of pumice in a fine-grained ash matrix. It has been quarried since at least 1893, though not on the present scale until 1954, and is sold as Hinuera Stone for cladding and other decorative uses. The stone is soft enough to be quarried by cutting with saws. One of the first houses built with Hinuera stone was the Bishop's House in Ponsonby in 1893. The Hinuera Gap, a geological feature stretching west and southwest from the locality towards Piarere, was in prehistoric times the path of the Waikato River, which had its outlet i ... [...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] |
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] |
Pākehā
Pākehā (or Pakeha; ; ) is a Māori term for New Zealanders primarily of European descent. Pākehā is not a legal concept and has no definition under New Zealand law. The term can apply to fair-skinned persons, or to any non-Māori New Zealander. Papa'a has a similar meaning in Cook Islands Māori. Historically before the arrival of other ethnic groups the word Māori meant 'ordinary' or 'normal'. The arrival of Europeans led to the formation of a new term to distinguish the self-regarded 'ordinary' or 'normal' Māori from the new arrivals. The etymology of the word ''Pākehā'' remains unclear, but the term was in use by the late-18th century. In December 1814 the Māori children at Rangihoua in the Bay of Islands were "no less eager to see the ''packaha'' than the grown folks". In Māori, plural noun-phrases of the term include (the definite article) and (the indefinite article). When the word was first adopted into English, the usual plural was 'Pakehas'. However, spe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2006 New Zealand Census
The New Zealand Census of Population and Dwellings ( mi, Te Tatauranga o ngā Tāngata Huri Noa i Aotearoa me ō rātou Whare Noho) is a national population and housing census conducted by government department Statistics New Zealand every five years. There have been 34 censuses since 1851. In addition to providing detailed information about national demographics, the results of the census play an important part in the calculation of resource allocation to local service providers. The 2018 census took place on Tuesday 6 March 2018. The next census is expected in March 2023. Census date Since 1926, the census has always been held on a Tuesday and since 1966, the census always occurs in March. These are statistically the month and weekday on which New Zealanders are least likely to be travelling. The census forms have to be returned by midnight on census day for them to be valid. Conducting the census Until 2018, census forms were hand-delivered by census workers during the lead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2013 New Zealand Census
The 2013 New Zealand census was the thirty-third national census. "The National Census Day" used for the census was on Tuesday, 5 March 2013. The population of New Zealand was counted as 4,242,048, – an increase of 214,101 or 5.3% over the 2006 census. The 2013 census forms were the same as the forms developed for the 2011 census which was cancelled due to the February 2011 major earthquake in Christchurch. There were no new topics or questions. New Zealand's next census was conducted in March 2018. Collection methods The results from the post-enumeration survey showed that the 2013 census recorded 97.6 percent of the residents in New Zealand on census night. However, the overall response rate was 92.9 percent, with a non-response rate of 7.1 percent made up of the net undercount and people who were counted in the census but had not received a form. Results Population and dwellings Population counts for New Zealand regions. Note: All figures are for the census usually r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand State Highway 1
State Highway 1 (SH 1) is the longest and most significant road in the New Zealand road network, running the length of both main islands. It appears on road maps as SH 1 and on road signs as a white number 1 on a red shield, but it has the official designations SH 1N in the North Island, SH 1S in the South Island. SH 1 is long, in the North Island and in the South Island. Since 2010 new roads have reduced the length from . For the majority of its length it is a two-lane single carriageway, with at-grade intersections and property accesses, in both rural and urban areas. These sections have some passing lanes. Around of SH 1 is of motorway or expressway standard : in the North Island and in the South Island. Route North Island (SH 1N) SH 1 starts at Cape Reinga, at the northwestern tip of the Aupouri Peninsula, and since April 2010 has been sealed (mainly with either chipseal or asphalt) for its entire length. From Waitiki Landing south of Cape Reinga, SH 1 trav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitoa River
Waitoa is a settlement in the Matamata-Piako District of New Zealand. State Highway 26 runs through the town, and connects to Te Aroha 10 km to the north-east. A Fonterra dairy factory is a prominent blue building in the middle of the town. The Waitoa River runs through the village and is prone to flooding. A railway line runs to the dairy factory, and used to go to Te Aroha, however this section was closed and the line only runs to service the dairy factory. Two freezing works and a rendering plant also operate in the Waitoa area. Workers commute from nearby towns of Te Aroha, Morrinsville and Matamata. Demographics Statistics New Zealand describes Waitoa as a rural settlement, which covers . Waitoa is part of the larger Waitoa-Ngarua statistical area. Waitoa had a population of 291 at the 2018 New Zealand census, an increase of 6 people (2.1%) since the 2013 census, and unchanged since the 2006 census. There were 114 households, comprising 144 males and 150 females, gi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oruanui Eruption
The Oruanui eruption of New Zealand's Taupō Volcano (also known as the Kawakawa eruption or Kawakawa/Oruanui event) was the world's most recent Supervolcano#Known supereruptions, supereruption.} Eruption With a Volcanic Explosivity Index of 8, it is one of the largest eruptions ever to occur in New Zealand. It occurred about 26,500 years ago in the Late Pleistocene and generated approximately of pyroclastic fall deposits, of pyroclastic density current (PDC) deposits (mostly ignimbrite) and of primary intracaldera material, equivalent to of magma, totaling of total deposits. The eruption is divided into 10 different phases on the basis of nine geological map, mappable fall strata, units and a tenth, poorly preserved but volumetrically dominant fall unit. Modern-day Lake Taupō, in area and deep, partly fills the caldera generated during this eruption. A structural collapse is concealed beneath Lake Taupō, while the lake outline at least partly reflects volcano-tectonic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Thames
The Firth of Thames ( mi, Tikapa Moana-o-Hauraki) is a large bay located in the north of the North Island of New Zealand. It is the firth of the rivers Waihou and Piako, the former of which was formerly named the Thames River, and the town of Thames lies on its southeastern coast. Its Maori name is ''Tikapa''. In traditional legend, the firth and the greater Hauraki Gulf are protected by a taniwha named Ureia, who takes the form of a whale. The firth lies at the southern end of the Hauraki Gulf, southeast of the city of Auckland. It occupies a rift valley or graben between the Coromandel Peninsula and Hunua Ranges, which continues into the Hauraki Plains to the south. Conservation The Firth of Thames is an important site for waders or shorebirds, and is listed as a wetland of international importance under the Ramsar Convention. The Miranda Shorebird Centre, operated by the Miranda Naturalists' Trust, is located on the Seabird Coast, on the western shore of the bay at M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato River
The Waikato River is the longest river in New Zealand, running for through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Wai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piarere
Piarere is a locality in the Waikato region of New Zealand's North Island. It is situated on State Highway 29 close to its junction with State Highway 1, close to the shore of Lake Karapiro. The nearest towns are Tīrau, six kilometres to the southeast, Matamata, 10 kilometres to the northeast, and Cambridge, 10 kilometres to the northwest. The meaning of the settlement's name is uncertain, as ''piarere'' may be translated from Māori in numerous ways, but it is possibly a personal name.Reed, A.W. (1975). ''Place names of New Zealand''. Wellington: A.H. & A.W. Reed. p. 327 The Hinuera Gap, a geological feature stretching northeast of Piarere, was in prehistoric times the path of the Waikato River, which had its outlet in the Firth of Thames The Firth of Thames ( mi, Tikapa Moana-o-Hauraki) is a large bay located in the north of the North Island of New Zealand. It is the firth of the rivers Waihou and Piako, the former of which was formerly named the Thames River, and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
