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2011 Canterbury 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 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. Scientists classified it as an intraplate earthquake and a potential aftershock of the September 2010 Canterbury earthquake. Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the 2010 Canterbury earthquake 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cathedral Of The Blessed Sacrament, Christchurch
The Cathedral of the Blessed Sacrament, sometimes referred to as the Christchurch Basilica or the Catholic Cathedral, was a Catholic cathedral on Barbadoes Street in central Christchurch, New Zealand. It was the mother church of the Roman Catholic Diocese of Christchurch and seat of the Bishop of Christchurch. It was not a basilica, despite sometimes being referred to as one: the term was used because its design was similar to some European basilicas. Designed by architect Francis Petre, it was generally held to be the finest Renaissance Revival architecture, renaissance-style building in New Zealand.archINFORM website (retrieved 20 July 2012) On 7 April 1983, the building was registered as a Category I heritage item by the Heritage New Zealand, New Zealand Historic Places Trust, with the registration number 47. It was regarded a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Disasters In New Zealand By Death Toll
This is a list of New Zealand disasters by death toll, listing major peacetime disasters which occurred in New Zealand and its territories or involved a significant number of New Zealand citizens, in a specific incident, where the loss of life was 10 or more. 100 or more deaths File:DC-10 of Air New Zealand at Heathrow - 1977.jpg, Air New Zealand Flight 901 in 1979 File:1931 Hawkes Bay Earthquake - Town Hall, Napier (24529620482).jpg, Napier Town Hall following the earthquake File:The Wreck of HMS Orpheus on Manukau Bar, New Zealand ILN-1863.jpg, Illustration of the HMS ''Orpheus'' wreck File:Christ Church Cathedral - 2011 earthquake damage.jpg, Christchurch Cathedral following the earthquake File:TangiwaiMemorialPlaque1b.jpg, Tangiwai memorial plaque File:Wreck of the Tararua.jpg, Illustration of the SS ''Tararua'' wreck File:SS Wairarapa Wreck At Miners Head.jpg, SS ''Wairarapa'' wreck File:Charles-Blomfield-Mount-Tarawera-in-eruption-June-10-1886.jpg, Illustration of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Press
''The Press'' () is a daily newspaper published in Christchurch, New Zealand, owned by media business Stuff (company), Stuff Ltd. First published in 1861, the newspaper is the largest circulating daily in the South Island and publishes Monday to Saturday. One community newspaper—''Northern Outlook''—is also published by ''The Press'' and is free. The newspaper has won the title of New Zealand Newspaper of the Year (in its circulation category) three times: in 2006, 2007 and 2012. It has also won the overall Newspaper of the Year title twice: in 2006 and 2007. History Origins James FitzGerald (New Zealand politician), James FitzGerald came to Lyttelton, New Zealand, Lyttelton on the ''Charlotte Jane'' in December 1850, and was from January 1851 the first editor of the ''Lyttelton Times'', Canterbury, New Zealand, Canterbury's first newspaper. From 1853, he focussed on politics and withdrew from the ''Lyttelton Times''. After several years in England, he returned to Cante ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a Fracture (geology), planar fracture or discontinuity in a volume of Rock (geology), rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust (geology), crust result from the action of Plate tectonics, plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction, subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the Plane (geometry), plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geological maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geoscience Australia
Geoscience Australia is a statutory agency of the Government of Australia that carries out geoscientific research. The agency is the government's technical adviser on aspects of geoscience, and serves as the repository of geographic and geological data collated by the Commonwealth. On a user pays basis, the agency offers geospatial services, including topographic maps and satellite imagery. It is also a major contributor to the Australian Government's free, open data collections such as and . Strategic priorities The agency has six strategic priority areas: # building Australia's resource wealth in order to maximise benefits from Australia's minerals and energy resources, now and into the future; # ensuring Australia's community safety so that Australian communities are more resilient to natural hazards; # securing Australia's water resources in order to optimise and sustain the use of Australia's water resources; # managing Australia's marine jurisdictions in order to m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
GNS Science
GNS Science (), officially registered as the Institute of Geological and Nuclear Sciences Limited, is a New Zealand Crown Research Institute. It focuses on geology, geophysics (including seismology and volcanology), and nuclear science (particularly ion-beam technologies, isotope science and carbon dating). From 1 July 2025 GNS Science will become part of the new Public Research Organisation New Zealand Institute for Earth Science. Functions and responsibilities As well as undertaking basic research, and operating the national geological hazards monitoring network ( GeoNet) and the National Isotope Centre (NIC), GNS Science contracts its services to various private groups (notably energy companies) both in New Zealand and overseas, as well as to central and local government agencies, to provide scientific advice and information. GNS Science has its head office in Avalon, Lower Hutt, with other facilities in Gracefield, Dunedin, Wairakei, Auckland and Tokyo Tokyo, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aftershock
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in Epicenter, the same area of the Mainshock, main shock, caused as the displaced Crust (geology), 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 #Aftershock size and frequency with time, 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 d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seismological Society Of America
The Seismological Society of America (SSA) is an international Learned society, scientific society devoted to the advancement of seismology and the understanding of earthquakes for the benefit of society. Founded in 1906, the society has members throughout the world representing seismologists and other geophysicists, geologists, engineers, insurers, and policy-makers in preparedness and safety. History The society was established by academic, government, and other scientific and engineering professionals in the months following the April 18th 1906 San Francisco earthquake, San Francisco earthquake, with the first meeting of the Board of Directors taking place on December 1, 1906. Publications The Seismological Society of America publishes the ''Bulletin of the Seismological Society of America'' (''BSSA''), a journal of research in earthquake seismology and related disciplines since 1911, and ''Seismological Research Letters'' (''SRL''), which serves as a forum for informal co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intraplate Earthquake
An intraplate earthquake occurs in the ''interior'' of a Plate tectonics, tectonic plate, in contrast to an interplate earthquake on the ''boundary'' of a tectonic plate. They are relatively rare compared to the more familiar interplate earthquakes. Buildings far from plate boundaries are rarely protected with seismic retrofitting, so large intraplate earthquakes can inflict heavy damage. Examples of damaging intraplate earthquakes are the devastating 2001 Gujarat earthquake, the 2011 Christchurch earthquake, the 2012 Indian Ocean earthquakes, the 2017 Puebla earthquake, the 1811–1812 New Madrid earthquakes, and the 1886 Charleston earthquake. An earthquake that occurs within a subducting plate is known as an intraslab earthquake. Description The Earth's Crust (geology), crust is made up of seven primary and eight secondary Plate tectonics, tectonic plates, plus dozens of tertiary microplates. The large plates move very slowly on top of convection currents in the underlying Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reserve Bank Of New Zealand
The Reserve Bank of New Zealand (RBNZ) () is the central bank of New Zealand. It was established in 1934 and is currently constituted under the ''Reserve Bank of New Zealand Act 2021''. The current acting governor of the Reserve Bank, Christian Hawkesby, is responsible for New Zealand's currency and operating monetary policy. History The Reserve Bank of New Zealand was established from 1 August 1934 by the ''Reserve Bank of New Zealand Act 1933''. The Reserve Bank first issued banknotes in 1934, see New Zealand pound. The ''Banking (Prudential Supervision) Act 1989'', which came into effect in February 1990, resulted in the Reserve Bank becoming independent of government control in RBNZ's role of managing monetary policy by introducing an inflation targeting mandate. New Zealand was the first country in the world to try this regime, which was later adopted in other countries. The ''Reserve Bank of New Zealand Amendment Act 2008'' included amendments to the ''BPSA 1989'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Disasters By Cost
Disasters can have high costs associated with responding to and recovering from them. This page lists the estimated economic costs of relatively recent disasters. The costs of disasters vary considerably depending on a range of factors, such as the geographical location where they occur. When a large disaster occurs in a wealthy country, the financial damage may be large, but when a comparable disaster occurs in a poorer country, the actual financial damage may appear to be relatively small. This is in part due to the difficulty of measuring the financial damage in areas that lack insurance. For example, the 2004 Indian Ocean earthquake and tsunami, with a death toll of around 230,000 people, cost a "mere" $15 billion, whereas in the Deepwater Horizon oil spill, in which 11 people died, the damage was six times higher. The most expensive disaster in human history is the Chernobyl disaster, costing an estimated $700 billion. Chernobyl's circumstances make it a unique but particul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wellington
Wellington is the capital city of New Zealand. It is located at the south-western tip of the North Island, between Cook Strait and the Remutaka Range. Wellington is the third-largest city in New Zealand (second largest in the North Island), and is the administrative centre of the Wellington Region. It is the world's southernmost capital of a sovereign state. Wellington features a temperate maritime climate, and is the world's windiest city by average wind speed. Māori oral tradition tells that Kupe discovered and explored the region in about the 10th century. The area was initially settled by Māori iwi such as Rangitāne and Muaūpoko. The disruptions of the Musket Wars led to them being overwhelmed by northern iwi such as Te Āti Awa by the early 19th century. Wellington's current form was originally designed by Captain William Mein Smith, the first Surveyor General for Edward Wakefield's New Zealand Company, in 1840. Smith's plan included a series of inter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
