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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, where the plates are not subducting and the forces are accommodated in different ways. The largest city within the highest-risk zone is the nat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Active Fault
An active fault is a fault that is likely to become the source of another earthquake sometime in the future. Geologists commonly consider faults to be active if there has been movement observed or evidence of seismic activity during the last 10,000 years. * Active faulting is considered to be a geologic hazard - one related to earthquakes as a cause. Effects of movement on an active fault include strong ground motion, surface faulting, tectonic deformation, landslides and rockfalls, liquefaction, tsunamis, and seiches. Quaternary faults are those active faults that have been recognized at the surface and which have evidence of movement during the Quaternary Period. Related geological disciplines for ''active-fault'' studies include geomorphology, seismology, reflection seismology, plate tectonics, geodetics and remote sensing, risk analysis, and others. Location Active faults tend to occur in the vicinity of tectonic plate boundaries, and active fault research has foc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1855 Wairarapa Earthquake
The 1855 Wairarapa earthquake occurred on 23 January at about 9.17 p.m., affecting much of the Cook Strait area of New Zealand, including Marlborough in the South Island and Wellington and the Wairarapa in the North Island. In Wellington, close to the epicentre, shaking lasted for at least 50 seconds. The moment magnitude of the earthquake has been estimated as 8.2, the most powerful recorded in New Zealand since systematic European colonisation began in 1840. This earthquake was associated with the largest observed movement on a strike-slip fault, maximum . It has been suggested that the surface rupture formed by this event helped influence Charles Lyell to link earthquakes with rapid movement on faults. Tectonic setting New Zealand lies along the boundary between the Australian and Pacific Plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paraparaumu
Paraparaumu () is a town in the south-western North Island of New Zealand. It lies on the Kapiti Coast, north of the nation's capital city, Wellington. Like other towns in the area, it has a partner settlement at the coast called Paraparaumu Beach, which lies directly opposite Kapiti Island. The two towns form part of the Kapiti Coast District. Together with the nearby Raumati Beach and Raumati South they are among the fastest-growing urban areas in New Zealand, and are major dormitory towns with workers commuting to the cities that make up the Wellington urban area. The four towns between them have a 2012 population of over 49,000 people. Inland behind Paraparaumu is the Maungakotukutuku area. Paraparaumu is a Māori-language name meaning "scraps from an earth oven"; means "dirt" or "scraps", and means "oven". The village of Lindale is a located just north of the Paraparaumu town centre. It began as a Tourist and Agricultural Centre, but later gained a reputation for cheese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manawatū-Whanganui
Manawatū-Whanganui (; spelled Manawatu-Wanganui prior to 2019) is a region in the lower half of the North Island of New Zealand, whose main population centres are the cities of Palmerston North and Whanganui. It is administered by the Manawatū-Whanganui Regional Council, which operates under the name Horizons Regional Council. Name In the Māori language, the name is a compound word that originates from an old Māori waiata (song). The waiata describes the search by an early ancestor, Haunui-a-Nanaia, for his wife, during which he named various waterways in the district, and says that his heart () settled or momentarily stopped () when he saw the Manawatu River. ''Whanga nui'' is a phrase meaning "big bay" or "big harbour". The first name of the European settlement at Whanganui was ''Petre'' (pronounced Peter), after Lord Petre, an officer of the New Zealand Company, but the name was never popular and was officially changed to "Wanganui" in 1854. In the local dialect, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1835 Auckland Earthquake
The 1835 Auckland earthquake was a magnitude 6.5 earthquake that occurred sometime during 1835 in the Auckland region of New Zealand. The earthquake was caused by movement along the Wairoa North Fault, which runs through the area. At the time, the settlement of Auckland was still quite small, and there are limited records of the specific damage caused by the earthquake. However, historical accounts suggest that the earthquake caused significant shaking and rumbling in the area, and it is possible that some buildings or structures may have been damaged or collapsed. Despite this, there are no records of major damage or casualties resulting from the earthquake. The 1835 Auckland earthquake remains an important event in the region's history, particularly as it highlights the seismic activity that can occur in the area due to the presence of faults such as the Wairoa North Fault. Earthquake The earthquake shock was felt as far away as Kaitaia and New Plymouth. However, due to the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland
Auckland (pronounced ) ( mi, Tāmaki Makaurau) is a large metropolitan city in the North Island of New Zealand. The List of New Zealand urban areas by population, most populous urban area in the country and the List of cities in Oceania by population, fifth largest city in Oceania, Auckland has an urban population of about It is located in the greater Auckland Region—the area governed by Auckland Council—which includes outlying rural areas and the islands of the Hauraki Gulf, and which has a total population of . While European New Zealanders, Europeans continue to make up the plurality of Auckland's population, the city became multicultural and Cosmopolitanism, cosmopolitan in the late-20th century, with Asian New Zealanders, Asians accounting for 31% of the city's population in 2018. Auckland has the fourth largest Foreign born, foreign-born population in the world, with 39% of its residents born overseas. With its large population of Pasifika New Zealanders, the city is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Auckland
South Auckland is an imprecisely defined urban area of Auckland, New Zealand, with a young population, a relatively large Polynesian and Māori demographic, and lower incomes than other parts of Auckland. The name ''South Auckland'', though not an official place name, has come into common use For example: among New Zealanders. It also appears in the names of some organisations and companies. Since the 1970s the term "South Auckland" has developed negative connotations with outsiders, being associated with deprivation, crime and violence. When street crime occurs in the area, the mass media tend to use the generic "South Auckland" phrase, with its vague and unfortunate stereotypes, rather than a more precise name of a suburb or territorial authority. Barry Curtis, mayor of Manukau City from 1983 to 2007, tried to discourage use of the name "South Auckland" because of its negative connotations. History The area between Manurewa and Clevedon was historically a large swampland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taranaki
Taranaki is a region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano of Mount Taranaki, also known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is home to more than 65 per cent of the population of Taranaki. New Plymouth is in North Taranaki along with Inglewood and Waitara. South Taranaki towns include Hāwera, Stratford, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is the second highest mountain in the North Island, and the dominant geographical feature of the region. A Māori legend says that Mount Taranaki previously lived with the Tongariro, Ngaur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Plymouth
New Plymouth ( mi, Ngāmotu) is the major city of the Taranaki region on the west coast of the North Island of New Zealand. It is named after the English city of Plymouth, Devon from where the first English settlers to New Plymouth migrated. The New Plymouth District, which includes New Plymouth City and several smaller towns, is the 10th largest district (out of 67) in New Zealand, and has a population of – about two-thirds of the total population of the Taranaki Region and % of New Zealand's population. This includes New Plymouth City (), Waitara (), Inglewood (), Ōakura (), Ōkato (561) and Urenui (429). The city itself is a service centre for the region's principal economic activities including intensive pastoral activities (mainly dairy farming) as well as oil, natural gas and petrochemical exploration and production. It is also the region's financial centre as the home of the TSB Bank (formerly the Taranaki Savings Bank), the largest of the remaining non-governm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haowhenua Earthquake
The Haowhenua (Māori for 'land swallower') earthquake was a large earthquake that occurred around 1460 AD causing uplift to parts of Wellington, New Zealand. In his 1923 work ''Miramar Island and its History'', Elsdon Best recounted Māori stories handed down through generations about early settlement in Wellington and the uplifting of Miramar. The present entrance to Wellington Harbour was called Te Au-a-Tane and the western channel (now the Rongotai isthmus) was called Te-Awa-a-Taia. Between the two channels sat the island of Motu-Kairangi (present day Miramar Peninsula). Elsdon stated:I obtained from Maori sources a story to the effect that, in the time of Te Ao-haere-tahi, who flourished eighteen generations ago, a violent earthquake-shock so lifted these lands that the Awa-a-Taia channel became dry, and Motu-kairangi a part of the mainland. We have no means of verifying such oral traditions, but it may be correct, and the shock may have been the cause of the raised beaches t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wellington Region
Greater Wellington, also known as the Wellington Region (Māori: ''Te Upoko o te Ika''), is a non-unitary region of New Zealand that occupies the southernmost part of the North Island. The region covers an area of , and has a population of The region takes its name from Wellington, New Zealand's capital city and the region's seat. The Wellington urban area, including the cities of Wellington, Porirua, Lower Hutt, and Upper Hutt, accounts for percent of the region's population; other major urban areas include the Kapiti conurbation (Waikanae, Paraparaumu, Raumati Beach, Raumati South, and Paekākāriki) and the town of Masterton. Local government The region is administered by the Wellington Regional Council, which uses the promotional name Greater Wellington Regional Council. The council region covers the conurbation around the capital city, Wellington, and the cities of Lower Hutt, Porirua, and Upper Hutt, each of which has a rural hinterland; it extends up the west coa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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