Hornby Clocktower
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Hornby Clocktower
The Hornby Clocktower (also known as the Hornby Clock Tower or simply as the clock tower to local residents) was an iconic Christchurch building, situated in the suburb of Hornby on New Zealand State Highway 1. It marked the southern entrance to Christchurch for over 50 years. Less than three months after a full refurbishment in 2010, the building was damaged in the 2011 Christchurch earthquake and subsequent aftershocks. It was demolished by October 2014. History 1960s original building The original incarnation of the building was constructed some time during the 1960s, and was designed by Don Donnithorne. During its early usage, it was home to the Central Canterbury Electric Power Board. 2010 refurbishment The building was refurbished in 2010 and completed by December of that year. It had been redesigned by Wilson and Hill Architects and was managed by Epoch Property. The upper five floors of the tower were designated as office space. The ground level was reserved for r ...
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Clock Tower Building Hornby Christchurch New Zealand
A clock or a timepiece is a device used to measure and indicate time. The clock is one of the oldest human inventions, meeting the need to measure intervals of time shorter than the natural units such as the day, the lunar month and the year. Devices operating on several physical processes have been used over the millennia. Some predecessors to the modern clock may be considered as "clocks" that are based on movement in nature: A sundial shows the time by displaying the position of a shadow on a flat surface. There is a range of duration timers, a well-known example being the hourglass. Water clocks, along with the sundials, are possibly the oldest time-measuring instruments. A major advance occurred with the invention of the verge escapement, which made possible the first mechanical clocks around 1300 in Europe, which kept time with oscillating timekeepers like balance wheels., pp. 103–104., p. 31. Traditionally, in horology, the term ''clock'' was used for a str ...
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Christchurch
Christchurch ( ; mi, Ōtautahi) is the largest city in the South Island of New Zealand and the seat of the Canterbury Region. Christchurch lies on the South Island's east coast, just north of Banks Peninsula on Pegasus Bay. The Avon River / Ōtākaro flows through the centre of the city, with an urban park along its banks. The city's territorial authority population is people, and includes a number of smaller urban areas as well as rural areas. The population of the urban area is people. Christchurch is the second-largest city by urban area population in New Zealand, after Auckland. It is the major urban area of an emerging sub-region known informally as Greater Christchurch. Notable smaller urban areas within this sub-region include Rangiora and Kaiapoi in Waimakariri District, north of the Waimakariri River, and Rolleston and Lincoln in Selwyn District to the south. The first inhabitants migrated to the area sometime between 1000 and 1250 AD. They hunted moa, which led ...
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Hornby, New Zealand
Hornby is a major residential and retail suburb at the western edge of Christchurch, New Zealand. The suburb is directly connected to other parts of Christchurch and the South Island by a number of main arterial routes, including State Highway 1 and the Christchurch Southern Motorway. History European settlement During the early stages of European settlement, Hornby was originally referred to as Southbridge Junction – with the junction acting as the start of the main road south. Due to rising confusion with the nearby town of Southbridge, a decision was made to rename the area to Hornby in 1878, although the origins of this name are unclear. One explanation holds that the suburb was named after Hornby-with-Farleton in Lancashire by Frederick William Delamain, who came to Christchurch from England in 1852. Delamain owned a nearby homestead, which gave its name to the nearby suburb of Yaldhurst, and was a prominent figure in the area during the latter half of the 19th centur ...
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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 trav ...
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2011 Christchurch Earthquake
A major earthquake occurred in Christchurch on Tuesday 22 February 2011 at 12:51 p.m. local time (23:51 UTC, 21 February). The () earthquake struck the entire of the Canterbury region in the South Island, centred south-east of the central business district. It caused widespread damage across Christchurch, killing 185 people, in New Zealand's fifth-deadliest disaster. Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the magnitude 7.1 Canterbury earthquake of 4 September 2010 and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was felt across the South Island and parts of the lower and central North Island. While the initial quake only lasted for approximately 10 seconds, the damage was severe because of the location and shallowness of the earthquake's focus in relation to Christchurch as well as ...
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Aftershock
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to a consistent pattern. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms. Distribution of aftershocks Most aftershocks are located over the full area of fault rupture and either occur along the fault plane itself or along other faults within the volume affected by the strain associated with the main shock. Typically, aftershocks are found up to a distance equal to the rupture length away from the fault plane. The pattern ...
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Don Donnithorne
Donald Ewart Donnithorne (31 July 1926 – 5 August 2016) was a New Zealand architect based in Christchurch. Born on 31 July 1926, and raised in Timaru, Donnithorne was the son of hotelkeepers. Following World War II he studied architecture by correspondence in the "Christchurch Atelier"', instead of travelling to the only architecture school in New Zealand at that time in Auckland. His student contemporaries included Miles Warren and Peter Beaven, and the three would go on to become the most significant figures in Christchurch architecture of the second half of the 20th century, producing works with clean, modernist lines. However, unlike Warren and Maurice Mahoney, who were strongly influenced by brutalism, Donnithorne followed Scandinavian cues in his work. One of Donnithorne's earliest designs was for the Evangelistic Temple, at the corner of Colombo Street and Moorhouse Avenue in Christchurch. His later works included the Wigram Air Force Museum, the Netball Centre in H ...
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List Of Coffeehouse Chains
This list of notable coffeehouse chains catalogues the spread and markets share of coffeehouses world-wide. This list excludes the many companies which operate coffeeshops within retail establishments, notably bookstores and department stores, or restaurants or convenience stores which also serve coffee. These chains frequently engage in coffee wars to gain brand and consumer market share. Starbucks, Dunkin', and Tim Hortons are the three largest coffee companies in the world, respectively. The largest coffee houses typically have substantial supply-chain relations with the world's major coffee-producing countries. They collectively wield prominent influence in global coffee economics by setting commodity prices, maintaining value chains, and supporting developing economics. List See also * Coffee wars * List of bakery cafés * List of coffee companies * List of doughnut shops * Lists of restaurants References {{Companies by industry * Coffeehouse A coffeehouse, ...
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Strip Mall
A strip mall, strip center or strip plaza is a type of shopping center common in North America where the stores are arranged in a row, with a sidewalk in front. Strip malls are typically developed as a unit and have large parking lots in front. Many of them face major traffic arterials and tend to be self-contained with few pedestrian connections to surrounding neighborhoods. Smaller strip malls may be called mini-malls, while larger ones may be called power centers or big box centers. In 2013, ''The New York Times'' reported that the United States had 65,840 strip malls. In 2020, ''The Wall Street Journal'' wrote that in the United States, despite the continuing retail apocalypse starting around 2010, investments and visitor numbers were increasing to strip malls. In the United Kingdom and Ireland, strip malls are called retail parks or retail outlets. They are usually located on the outskirts of most towns and cities, and serve as an alternative to the High Street in the UK ...
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Hornby Clocktower Demolition
Hornby may refer to: Places In England * Hornby, Lancashire * Hornby, Hambleton, village in North Yorkshire * Hornby, Richmondshire, village in North Yorkshire Elsewhere * Hornby, Ontario, community in the town of Halton Hills, Ontario, Canada * Hornby Island, island in British Columbia, Canada * Hornby, New York, town * Hornby, New Zealand, suburb of Christchurch Other * Hornby (surname) * Hornby Railways, popular British brand of model railway * SS ''Hornby'', a 1908 tug tender See also * Hornby Castle (other) * Hornby Dock, dock in Liverpool, England * Hornby Lighthouse, in New South Wales, Australia * Hornby Priory, former monastery in Hornby, Lancashire, England * Hornby School, historic school house in Pennsylvania * Hornby High School, Christchurch, New Zealand * Hornsby (other) Hornsby may refer to: Places * Hornsby, Cumbria, a List of places in Cumbria, place in Cumbria, Northern England * Hornsby, New South Wales, a suburb of Sydn ...
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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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Aftershocks
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to a consistent pattern. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms. Distribution of aftershocks Most aftershocks are located over the full area of fault rupture and either occur along the fault plane itself or along other faults within the volume affected by the strain associated with the main shock. Typically, aftershocks are found up to a distance equal to the rupture length away from the fault plane. The pattern ...
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