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Hororata
Hororata is a village at the northwestern edge of the Canterbury Plains in the South Island of New Zealand. It is located 15 kilometres southwest of Darfield, New Zealand, Darfield, five kilometres south of Glentunnel, and 50 kilometres west of Christchurch, on the banks of the Hororata River. Hororata, when translated from Māori language, Maori means "drooping rata". There are a large number of rata growing in the district. History Hororata developed as a village to service the local farming community. In the early 1900s, the village had all the services that a small town would expect. These include a hotel, a Presbyterian and an St John's Church, Hororata, Anglican church, stores, a school, post office, flour mill and a brewery. There was a large blacksmiths shop with a total of five forges. Early European New Zealand pioneer John Studholme and his wife lived at Terrace Station on Milnes Road before selling the run to John Hall (New Zealand politician), John Hall ...
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St John's Church, Hororata
St John's Church, Hororata also known as St John's Memorial Church and the Hororata Memorial Church is an Anglican church located in Hororata, New Zealand. History St John's Hall The first building to be built on the site was a small wooden church, which was built in 1875. On 23 June 1983, the wooden church was registered by the New Zealand Historic Places Trust as a Category 2 historic place, with the registration number being 1785. The building was later moved across the road to its present day location for the construction of the current stone church. Meanwhile, the 1881 wooden church had become the parish hall, but since the 2010 Canterbury earthquake it has been used for services. St John's Church On 6 February 1910, the stone church had its foundation stone laid and the building consecrated on 27 February 1911. The funds were bequested by former New Zealand Premier (Prime Minister), Sir John Hall as a memorial for his late wife, Rose, Lady Hall. The new chur ...
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2010 Canterbury Earthquake
The 2010 Canterbury earthquake (also known as the Darfield earthquake) struck the South Island of New Zealand with a moment magnitude of 7.1 at on , and had a maximum perceived intensity of X (''Extreme'') on the Mercalli intensity scale. Some damaging aftershocks followed the main event, the strongest of which was a magnitude 6.3 shock known as the Christchurch earthquake that occurred nearly six months later on 22 February 2011. Because this aftershock was centred very close to Christchurch, it was much more destructive and resulted in the deaths of 185 people. The earthquake on 4 September caused widespread damage and several power outages, particularly in the city of Christchurch, New Zealand's second largest city at that time. Two residents were seriously injured, one by a collapsing chimney and a second by flying glass. One person died of a heart attack suffered during the quake. Another person died after a fall during the quake. Mass fatalities were avoided partly due t ...
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Hororata River
The Hororata River is a river of Canterbury, in the South Island of New Zealand. A tributary of the Selwyn River, the Hororata has its sources in rough hill country north of Windwhistle, and flows east through the township of Hororata before reaching the Selwyn northwest of Dunsandel. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Canterbury, New Zealand Rivers of New Zealand {{CanterburyNZ-river-stub ...
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John Hall (New Zealand Politician)
Sir John Hall (18 December 1824 – 25 June 1907) was a New Zealand politician who served as the 12th premier of New Zealand from 1879 to 1882. He was born in Kingston upon Hull, England, the third son of George Hall, a captain in the navy. At the age of ten he was sent to school in Switzerland and his education continued in Paris and Hamburg. After returning to England and being employed by the Post Office, at the age of 27 he decided to emigrate. He was also Mayor of Christchurch. Migration to New Zealand After reading a book on sheep farming, Hall emigrated to New Zealand, on the ''Samarang'', arriving in Lyttelton on 31 July 1852. His brothers George and Thomas followed him to New Zealand soon after. He developed one of the first large scale sheep farming runs in Canterbury. Political offices In 1853, he was elected to the Canterbury Provincial Council. He would later rise through the ranks of magistrate, was the first town council Chairman in Christchurc ...
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Glentunnel
Glentunnel (previously known as Surveyors Gully) is a village located in the Selwyn District of the Canterbury region of New Zealand's South Island. It has a close historical association with coal, clay and sand mines of the Malvern area. Originally named ‘Surveyors Gully’, Glentunnel, derived from the tramway tunnel in the glen that gave access to the Homebush coal mine. Coal was discovered in 1871, along with deposits of fine clay, which lead to the establishment of a brick, tile and pottery works that survived until the 1980s. It is located on State Highway 77/ Inland Scenic Route 72, and is west from Darfield and west of Christchurch. History 1800s–2000s Glentunnel was served by the Whitecliffs Branch, a branch line railway, from the line's opening on 3 November 1875 through to its closure on 31 March 1962. However, the station was not open until 22 April 1876. Few remnants of the railway remain in the town, with the station's platform incorporated into ...
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George Williamson Hall
George Williamson Hall (7 September 1818 – 27 February 1896) was a 19th-century Member of Parliament in Christchurch, New Zealand. Biography George Hall was born in Sculcoates, Yorkshire, in 1818. He married Agnes Emma Dryden c. 1850 in Kingston upon Hull. He was the eldest brother of Sir John Hall, 12th Premier of New Zealand. George and Agnes Hall emigrated to Canterbury in 1853, arriving on the ''Royal Albert''; John Hall had emigrated a year before them. Agnes's sister, Rose Anne Dryden married John Hall in 1861 at Kingston upon Hull. Hall began his early life at sea, as a merchant seaman and after arriving in New Zealand, became a pastoralist. Hall stood for the Heathcote seat in the General Assembly in 1861 and defeated Feliz Wakefield comfortably. Political career The polling for the 1861 election in the Heathcote electorate took place on 12 February 1861. Hall and Edward Wakefield contested the election. Hall was a local resident with no prior political exper ...
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Selwyn River / Waikirikiri
The Selwyn River / Waikirikiri flows through the Selwyn District of Canterbury in the South Island of New Zealand. Description The river has its source in the Southern Alps and flows east for before emptying into Lake Ellesmere / Te Waihora, south of Banks Peninsula. Terrace cliffs above the river's upper reaches gave the town of Whitecliffs its name. For much of its course the river flows through wide shingle channels. In drought years, the river can disappear beneath this bed and seem to dry up completely. This frequently occurs where State Highway 1 crosses the river at the settlement of Selwyn, about upstream from its outflow into Lake Ellesmere. In the foothills, the Selwyn flows year-round. On the plains, the riverbed is highly permeable, and the river overlays a deep and porous aquifer. As soon as the river reaches the plains, water begins leaking down through the bed and into the aquifer. In most months, all river-water disappears within of leaving the foothills. ...
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John Studholme
John Studholme (1829–1903) was a 19th-century British pioneer of New Zealand, farmer and politician in the Canterbury region of New Zealand.Mosley, vol.3 p. 2803 Early life John Studholme was born in 1829 the son of John Studholme, a landowner in Cumberland, now part of Cumbria, England. He was educated at Sedbergh School and The Queen's College, Oxford, where he was a university scholar and earned a blue rowing in the university eight. At the age of 22, Studholme sailed to New Zealand with his two younger brothers Michael and Paul. Together they bought farmland in Selwyn and Rakaia. The following year, after having set up farms, they travelled to Australia to pursue the Victorian gold rush. Establishing settlement and farming In 1852, the Studholme brothers returned to New Zealand. Famously, they took a ship which only went as far as Nelson. Together they walked the 350 miles back to Christchurch. From this time on John and Michael began establishing large stations in both ...
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Selwyn District
Selwyn District is a predominantly rural district in central Canterbury, on the east coast of New Zealand's South Island. It is named after the Selwyn River / Waikirikiri, which is in turn named after Bishop George Selwyn, the first Anglican bishop of New Zealand who, in 1843 and 1844, travelled the length of the country by horse, foot, boat and canoe, leaving in his wake a sprinkling of locations that now bear his name. History The first inhabitants of the area were the Māori who first settled New Zealand from the Cook and Society Islands about 700 years ago. The predominant Māori tribe today, in Selwyn and most of the rest of the South Island, is Ngāi Tahu, whose local marae (meeting house) is at Taumutu near the exit of Lake Ellesmere (Te Waihora). In the late 19th century, European (chiefly British) colonists arrived and carved the area up into farmland. This has remained the predominant pattern ever since. The Selwyn District as a unit of government was formed in the ...
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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 ...
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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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Mercalli Intensity Scale
The Modified Mercalli intensity scale (MM, MMI, or MCS), developed from Giuseppe Mercalli's Mercalli intensity scale of 1902, is a seismic intensity scale used for measuring the intensity of shaking produced by an earthquake. It measures the effects of an earthquake at a given location, distinguished from the earthquake's inherent force or strength as measured by seismic magnitude scales (such as the "" magnitude usually reported for an earthquake). While shaking is caused by the seismic energy released by an earthquake, earthquakes differ in how much of their energy is radiated as seismic waves. Deeper earthquakes also have less interaction with the surface, and their energy is spread out across a larger volume. Shaking intensity is localized, generally diminishing with distance from the earthquake's epicenter, but can be amplified in sedimentary basins and certain kinds of unconsolidated soils. Intensity scales empirically categorize the intensity of shaking based on the effect ...
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