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Hinuera
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 ...
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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 W ...
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New Zealand State Highway 29
State Highway 29 (SH 29) is a New Zealand state highway that travels over the Kaimai Ranges linking the Bay of Plenty and Waikato regions. For most of its length, SH 29 is a two-lane single carriageway with occasional passing lanes and slow vehicle bays. 5 km of it near its eastern terminus is part of the Takitimu Drive Toll Road. Route SH 29 begins at SH 2 at a grade separated intersection at which only westbound SH 2 traffic can enter and eastbound traffic can exit. Immediately after it commences, SH 29 becomes the Takitimu Drive (Pyes Pa – Mount Maunganui Expressway) Toll Road. Before the eastern terminus was shifted to this route it was better known as 'Route K'. At the end of this tolled section, SH 29 reaches a roundabout intersecting the former eastern section (now SH 29A) and . SH 29 turns west through the village of Tauriko. From here SH 29 roughly follows the Wairoa River as it climbs the Kaimai Ranges. About a quarter of the way up the Kaimai's, SH 29 pa ...
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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-'' ireand ''imbri-'' ain Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when 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 density. Many pale i ...
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Hamilton, New Zealand
Hamilton ( mi, Kirikiriroa) is an inland city in the North Island of New Zealand. Located on the banks of the Waikato River, it is the seat and most populous city of the Waikato region. With a territorial population of , it is the country's fourth most-populous city. Encompassing a land area of about , Hamilton is part of the wider Hamilton Urban Area, which also encompasses the nearby towns of Ngāruawāhia, Te Awamutu and Cambridge. In 2020, Hamilton was awarded the title of most beautiful large city in New Zealand. The area now covered by the city was originally the site of several Māori villages, including Kirikiriroa, from which the city takes its Māori name. By the time English settlers arrived, most of these villages, which sat beside the Waikato River, were abandoned as a result of the Invasion of Waikato and land confiscation (''Raupatu'') by the Crown. Initially an agricultural service centre, Hamilton now has a diverse economy and is the third fastest growin ...
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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 t ...
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List Of Towns In New Zealand
This is a list of towns in New Zealand. The term " town" has no current statutory meaning in New Zealand, the few "Town Districts" having been abolished in 1989 or earlier. The list includes most urban areas in New Zealand. Those deemed urban areas by Statistics New Zealand (under either the NZSCA92 or SSGA18 standard) are marked with an asterisk. Isolated towns, such as Ashburton and Levin, are usually parts of a local government "District" (which occasionally has the same name), but the rest, such as Wainuiomata, Pukerua Bay, and Port Chalmers, are within city council boundaries, and are often referred to as suburbs of their respective cities. Many were boroughs during most of the twentieth century, and some earlier. __NOTOC__ A * Ahaura * Ahipara * Ahititi * Ahuroa * Aka Aka *Akaroa *Ākitio * Albany * Albert Town *Albury *Alexandra* * Allanton * Amberley* * Anakiwa * Arahiwi * Aramoana * Aranga * Arapohue * Arrowtown* *Arundel * Ashburton* * Ashhurst* *Ashley ...
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Matamata-Piako District
Matamata-Piako District is a local government area in the Waikato region of New Zealand. It lies to the east of the city of Hamilton. Geography The district encompasses the southern end of the Hauraki Plains and much of the Thames Valley, and is bounded in the east by the Kaimai Range. The rivers Piako and Waihou run through the district. The towns of Matamata, Morrinsville and Te Aroha are all within the district, with the Council's head office based in Te Aroha. The main industry in the region is dairy farming and Thoroughbred breeding and training. Other communities in the district include Mangateparu and Waitoa. Populated places Matamata-Piako District consists of the following towns, localities, settlements and communities: * Matamata Ward: ** Buckland ** Gordon ** Hinuera ** Matai ** Matamata ** Okauia South ** Okauia ** Paratu ** Peria ** Piarere ** Richmond Downs ** Selwyn ** Taihoa ** Tamihana ** Te Poi ** Turangaomoana ** '' Waharoa'' ** Walton ** ...
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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 commonly r ...
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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 tr ...
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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, ...
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Pumice
Pumice (), called pumicite in its powdered or dust form, is a volcanic rock that consists of highly vesicular rough-textured volcanic glass, which may or may not contain crystals. It is typically light-colored. Scoria is another vesicular volcanic rock that differs from pumice in having larger vesicles, thicker vesicle walls, and being dark colored and denser.Jackson, J.A., J. Mehl, and K. Neuendorf (2005) ''Glossary of Geology'' American Geological Institute, Alexandria, Virginia. 800 pp. McPhie, J., M. Doyle, and R. Allen (1993) ''Volcanic Textures A guide to the interpretation of textures in volcanic rocks'' Centre for Ore Deposit and Exploration Studies, University of Tasmania, Hobart, Tasmania..198 pp. Pumice is created when super-heated, highly pressurized rock is violently ejected from a volcano. The unusual foamy configuration of pumice happens because of simultaneous rapid cooling and rapid depressurization. The depressurization creates bubbles by lowering the solu ...
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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 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 mappable fall 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 collapse. Early eruption phases saw shifting vent pos ...
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