1901 Cheviot Earthquake
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1901 Cheviot Earthquake
The 1901 Cheviot earthquake occurred at 07:47 NZT on 16 November 1901 (20:15 15 November UTC) with an estimated magnitude of 6.9, centred near the township of Cheviot in the Canterbury region of New Zealand. Damage and casualties A baby was killed when a sod hut collapsed. Other casualties in the Canterbury region are not known. The ChristChurch Cathedral experienced some damage in this earthquake. The top of the spire fell again as a result of the 16 November 1901 Cheviot earthquake. This time, the stone construction was replaced with a more resilient structure of Australian hardwood sheathed with weathered copper sheeting, with an internal mass damper. Observations of sand blows (sand volcano) and lateral spreading, consistent with soil liquefaction phenomena in the township of Kaiapoi were reported in local newspapers in a two to three block area at the eastern end of Charles and Sewell Streets on the north bank of the Kaiapoi River, in addition to similar effects observ ...
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South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ...
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List Of Earthquakes In 1901
This is a list of earthquakes in 1901. Only magnitude 6.0 or greater earthquakes appear on the list. Exceptions to this are earthquakes which have caused death, injury or damage. Events which occurred in remote areas will be excluded from the list as they wouldn't have generated significant media interest. All dates are listed according to UTC time. The countries and their flags are noted as they would have appeared in this year for example the Netherlands being in control of present-day Indonesia. In all another year of below average activity. There was 15 magnitude 7.0+ events. Japan saw a great deal of activity this year. The majority of the 125 deaths came in China from an event in February. Overall By death toll * Note: At least 10 casualties By magnitude * Note: At least 7.0 magnitude Notable events January February March April May June August September October November December References {{Earthquakes in 1909 ...
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1901 Earthquakes
Nineteen or 19 may refer to: * 19 (number), the natural number following 18 and preceding 20 * one of the years 19 BC, AD 19, 1919, 2019 Films * ''19'' (film), a 2001 Japanese film * ''Nineteen'' (film), a 1987 science fiction film Music * 19 (band), a Japanese pop music duo Albums * ''19'' (Adele album), 2008 * ''19'', a 2003 album by Alsou * ''19'', a 2006 album by Evan Yo * ''19'', a 2018 album by MHD * ''19'', one half of the double album ''63/19'' by Kool A.D. * '' Number Nineteen'', a 1971 album by American jazz pianist Mal Waldron * ''XIX'' (EP), a 2019 EP by 1the9 Songs * "19" (song), a 1985 song by British musician Paul Hardcastle. * "Nineteen", a song by Bad4Good from the 1992 album ''Refugee'' * "Nineteen", a song by Karma to Burn from the 2001 album ''Almost Heathen''. * "Nineteen" (song), a 2007 song by American singer Billy Ray Cyrus. * "Nineteen", a song by Tegan and Sara from the 2007 album '' The Con''. * "XIX" (song), a 2014 song by Slipk ...
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1901 In New Zealand
The following lists events that happened during 1901 in New Zealand. Population A New Zealand census was held in March 1901. The population was given as 815,862, consisting of 43,112 Māori, 31 Moriori, and 772,719 others. – an increase in the non-Māori population of 9.86% over the previous census in 1896. The figures for the 1901 census revealed that the North Island's population had exceeded the South Island's for the first time since the Central Otago Gold Rush of 1861 – the two islands (plus their associated minor offshore islands) had populations of 390,579 and 382,140 respectively. Only 40% of the country's population was based in urban centres, and only two of these centres, Auckland and Dunedin, had populations of over 25,000. Incumbents Regal and viceregal *Head of State – Victoria (until 22 January), succeeded by Edward VII *Governor – The Earl of Ranfurly GCMG Government The 14th New Zealand Parliament continued. In government was the Liberal Party. *Speak ...
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Earthquakes In New Zealand
This is a list of large earthquakes that have occurred in New Zealand. Only earthquakes with a magnitude of 6.0 or greater are listed, except for a few that had a moderate impact. Aftershocks are not included, unless they were of great significance or contributed to a death toll, such as the M 6.3 2011 Christchurch earthquake and the M 7.3 aftershock to the 1931 Hawke's Bay earthquake. Earthquakes occur frequently in New Zealand as the country is situated in the collision zone between the Indo-Australian and Pacific tectonic plates, part of the Pacific Basin Ring of Fire, where many earthquakes and volcanoes occur. Most events occur along the main ranges running from Fiordland in the southwest to East Cape in the northeast. This axis follows the boundary between the Indo-Australian and Pacific plates. Large earthquakes are less common along the central Alpine Fault, where the plates are not subducting and the forces are accommodated in different ways. The largest city within ...
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Hurunui District
Hurunui District is a territorial local government district within the Canterbury Region on the east coast of New Zealand's South Island, north of Christchurch. It stretches from the east coast to the Main Divide. Its land area is . Local government During the period, 1853 to 1876, the area north of the Hurunui River was administered as part of the Nelson Province. After the abolition of the provinces in 1876 the Amuri and Cheviot counties were formed. In the 1989 local government reforms, these counties were merged with Hurunui County to form the present district. The current district mayor is Marie Black, who was elected in 2019 upon the retirement of previous mayor Winton Dalley. Population Hurunui District covers and had an estimated population of as of with a population density of people per km2. Hurunui District had a population of 12,558 at the 2018 New Zealand census, an increase of 1,029 people (8.9%) since the 2013 census, and an increase of 2,082 people ...
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Otago Witness
The ''Otago Witness'' was a prominent illustrated weekly newspaper in the early years of the European settlement of New Zealand, produced in Dunedin, the provincial capital of Otago. Published weekly it existed from 1851 to 1932. The introduction of the Otago Daily Times followed by other daily newspapers in its circulation area lead it to focus on serving a rural readership in the lower South Island where poor road access prevented newspapers being delivered daily. It also provided an outlet for local fiction writers. It is notable as the first newspaper to use illustrations and photographs and was the first New Zealand newspaper to provide a correspondence column for children, which was known as "Dot's Little Folk". Together with the Auckland based ''Weekly News'' and the Wellington based ''New Zealand Free Lance'' it was one of the most significant illustrated weekly New Zealand newspapers in the 19th and early 20th centuries. History Background Nine months after the first immi ...
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List Of Earthquakes In New Zealand
This is a list of large earthquakes that have occurred in New Zealand. Only earthquakes with a magnitude of 6.0 or greater are listed, except for a few that had a moderate impact. Aftershocks are not included, unless they were of great significance or contributed to a death toll, such as the M 6.3 2011 Christchurch earthquake and the M 7.3 aftershock to the 1931 Hawke's Bay earthquake. Earthquakes occur frequently in New Zealand as the country is situated in the collision zone between the Indo-Australian and Pacific tectonic plates, part of the Pacific Basin Ring of Fire, where many earthquakes and volcanoes occur. Most events occur along the main ranges running from Fiordland in the southwest to East Cape in the northeast. This axis follows the boundary between the Indo-Australian and Pacific plates. Large earthquakes are less common along the central Alpine Fault, where the plates are not subducting and the forces are accommodated in different ways. The largest city wit ...
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Kaiapoi
Kaiapoi is a town in the Waimakariri District of the Canterbury region, in the South Island of New Zealand. The town is located approximately 17 kilometres north of central Christchurch, close to the mouth of the Waimakariri River. It is considered a satellite town of Christchurch and is part of the Christchurch functional urban area. Kaiapoi is known for its substantial precolonial pā, established by powerful Kāi Tahu nobleman Tūrākautahi. One of the sons of the powerful rangatira Tūāhuriri, Tūrākautahi exerted vast influence over historical Ōtautahi (the site of modern-day Christchurch). His family controlled the pā he established in the area until it was sacked in 1830. The pā was one of the greatest centre of knowledge, economics and natural resources, with a highly complex social structure. All decisions were undertaken by the nobility, who consulted with highly skilled tohunga. In selecting the pā site, Tūrākautahi determined that food ( kai) would need ...
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Coordinated Universal Time
Coordinated Universal Time or UTC is the primary time standard by which the world regulates clocks and time. It is within about one second of mean solar time (such as UT1) at 0° longitude (at the IERS Reference Meridian as the currently used prime meridian) and is not adjusted for daylight saving time. It is effectively a successor to Greenwich Mean Time (GMT). The coordination of time and frequency transmissions around the world began on 1 January 1960. UTC was first officially adopted as CCIR Recommendation 374, ''Standard-Frequency and Time-Signal Emissions'', in 1963, but the official abbreviation of UTC and the official English name of Coordinated Universal Time (along with the French equivalent) were not adopted until 1967. The system has been adjusted several times, including a brief period during which the time-coordination radio signals broadcast both UTC and "Stepped Atomic Time (SAT)" before a new UTC was adopted in 1970 and implemented in 1972. This change also a ...
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Soil Liquefaction
Soil liquefaction occurs when a cohesionless saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress such as shaking during an earthquake or other sudden change in stress condition, in which material that is ordinarily a solid behaves like a liquid. In soil mechanics, the term "liquefied" was first used by Allen Hazen in reference to the 1918 failure of the Calaveras Dam in California. He described the mechanism of flow liquefaction of the embankment dam as: The phenomenon is most often observed in saturated, loose (low density or uncompacted), sandy soils. This is because a loose sand has a tendency to compress when a load is applied. Dense sands, by contrast, tend to expand in volume or 'dilate'. If the soil is saturated by water, a condition that often exists when the soil is below the water table or sea level, then water fills the gaps between soil grains ('pore spaces'). In response to soil compressing, the po ...
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Sand Volcano
Sand boils or sand volcanoes occur when water under pressure wells up through a bed of sand. The water looks like it is boiling up from the bed of sand, hence the name. Sand volcano A sand volcano or sand blow is a cone of sand formed by the ejection of sand onto a surface from a central point. The sand builds up as a cone with slopes at the sand's angle of repose. A crater is commonly seen at the summit. The cone looks like a small volcanic cone and can range in size from millimetres to metres in diameter. The process is often associated with soil liquefaction and the ejection of fluidized sand that can occur in water-saturated sediments during an earthquake. The New Madrid Seismic Zone exhibited many such features during the 1811–12 New Madrid earthquakes. Adjacent sand blows aligned in a row along a linear fracture within fine-grained surface sediments are just as common, and can still be seen in the New Madrid area. In the past few years, much effort has gone into ...
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