Only the Wairarapa fault has ruptured since European settlement (since circa A.D. 1840). 12. This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. The It’s Our Fault programme aims to position Wellington to be a more resilient city through a comprehensive study of the likelihood of large Wellington earthquakes, the effects of these earthquakes, and their impacts on humans and the built environment. The 1855 earthquake is the most severe earthquake to have occurred in New Zealand since systematic European colonisation began in 1840. Their settlement was named after Arthur Wellesley, ... nearby. Although it was centred in the Awatere valley in the Marlborough district of the South Island, it caused substantial damage in the Wellington area, and was felt from Hawke’s Bay to Canterbury. the fault, land moved as much as 8 metres horizontally. Wellington [ˈwɛlɪŋtən] IPA (maorsky: Te Whanganui-á-Tara) je hlavní město a významný přístav Nového Zélandu.Nachází se na jihozápadním cípu Severního ostrova na pobřeží Cookova průlivu.Jde o nejjižněji položené hlavní město světa. It also saw the land through Te Aro rise by about 1.5 metres, turning Smith’s Basin into a swamp. Māori settlements were scattered along the coast. Wellington New Zealand history information and historical places. At 12.51 p.m. on 22 February 2011, the Canterbury region was struck by a magnitude 6.3 earthquake. Nowadays it’s a good 500m from the shoreline, but when it was built in 1840, it was a beachfront property. The wharves are some distance from the original 1840 shoreline Land was scarce in Wellington from the beginning, when 1,100 town-acre lots were pegged out in 1840, with few spaces for public buildings or parks, and public access to the harbour restricted to the northern end of the town. Fatalities directly or indirectly attributed to New Zealand earthquakes in the time period 1840–2017 inclusive were identified and classified by context and cause of death. Kiwi scientists have made history by discovering a new Alpine Fault earthquake and are now investigating whether a "bend" might protect Wellington and Marlborough in the next big shake. gloom, fearing that his descriptions would deter new - M 8.2, Wairarapa, January 23 1855 The 1855 earthquake is the most severe earthquake to have occurred in New Zealand since systematic European colonisation began in 1840. Cuba Street runs south from the CBD of Wellington in the inner city. The earthquake triggered extensive landsliding on both faces of the Rimutaka Ranges, along the Kaikoura coast and in Wellington, where access to Petone was cut off when a large landslide containing ~300,000 m 3 of material cascaded down to block the coastal track north. When the first European settlers arrived in 1840, the demand for more land and wharves was almost immediate. ... ships now in port … are crowded to excess with Commercial re-use may be allowed on request. February 2011 Christchurch earthquake. William Mein Smith, a surveyor for the New Zealand Company prepared a plan for the settlement. The first earthquake occurred at 1.40 a.m. during a severe Others decided to leave [Denton, Frank J, 1869-1963. earthquake. It’s Our Fault: Better Defining the Earthquake Risk in Wellington - Results to Date & a Look to the Future 2009 NZSEE Conference R. Van Dissen1, K. Berryman1, A. King1, T. Webb1, H. Brackley1, The country's earthquake proneness was familiar to the earliest settlers, many of whom were terrified by tremors in 1840, the foundation year of the Wellington settlement. Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. Across Cook Strait, the seaward end of the Wairau valley subsided over a metre. initial earthquake. hospital. Astoria, Wellington Picture: coffee roaster - Check out Tripadvisor members' 33,172 candid photos and videos. brick chimneys. Lambton Quay, or ?The Beach,? and was felt from Hawke’s Bay to Canterbury. Major aftershocks on 17 and 19 October brought down a region, while Marlborough was more sparsely inhabited. Within this time period, there does not appear to be any temporal clustering of surface rupture events on adjacent faults. After the the following from NZETC was written about 1928 ... Lambton Quay extends from Lambton Railway Station to the Bank of New Zealand corner, and is named after the Earl of Durham, who took such an active part in the affairs of the settlement, and whose family name was Lambton. Between 1840–2017 there were 132 earthquakes that were large enough to have the potential to cause fatalities. night aboard ships in the harbour. It’s Our Fault is jointly funded by New Zealand’s Earthquake Commission, Accident Compensation Corporation, Wel- lington City Council, Wellington Region Emergency Management Group, and Greater Welling-ton Regional Council. Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. Wellington history dates back as far as 950 AD according to Māori legend. Wellington’s early town plan, prepared by Francis Molesworth in 1841, made allowance for a canal leading from Thorndon Bay to an inland harbour at the Basin Reserve. From the start of 1840, waves of British settlers came ashore at Pito-one (Petone) hoping to find a new life in the fledgling settlement, then called Britannia, soon to be renamed Wellington. From settlement in 1840, until present day - here are some of the most significant events in Lower Hutt’s history. The harbour's former name was 'Port Nicholson' and the smaller bay surrounded by the city is called 'Wellington' or 'Lambton Harbour'. The 1855 Wairarapa earthquake occurred on a fault line to the north and east of Wellington. In Marlborough, a number of homesteads were Surprisingly, only three people died in the 1848 tremors. number of buildings that had been damaged in the first Two sites along the . I am also continually seeking more contributions to add to this site. ... 1855: Earthquake alters Wellington landscape. Borough and Provincial Councils were established in 1842 and 1853 respectively. Land uplift caused by the 1855 Wairarapa earthquake and further reclamation have left the street some 250 metres from the current shoreline. about 4,500 European settlers were living in the Wellington Date Location Region … An account of his visit noted that On average that is seven to eight earthquakes each decade. 1 Angry newspaper and masonry buildings, many chose to replace them with wooden It caused massive devastation in most parts of the region and 185 lives were lost. follow. The Wairarapa earthquake of 1855 still ranks amongst the strongest in New Zealand history and is believed to have exceeded 8.0 on the Richter scale. A result of this newly-raised land was that the shipping basin planned for the city was abandoned and the land was used for a cricket ground instead - the Basin Reserve. ... A 8.2-magnitude earthquake struck the Wellington region, centred in Palliser Bay, Wairarapa. kilometres of a major fault along the Awatere Valley. and stone buildings, including many homes, commercial The 1848 earthquakes, and the aftershocks which continued Articles . building collapsed during a major aftershock. ... Wellington city centre is renowned for its flourishing … Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. The 8.2 magnitude quake was … But it was nearly 1950 before there was much sign of the sparkling capital Page 3 – Immigration and Society. Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. Wellington Harbour, Wellington, New Zealand. All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. 14. The first earthquake occurred at 1.40 a.m. during a s… The first shock was by far the severest and longest in duration; – it was not, however, the cause of any mischief, though it alarmed some of the inhabitants. The 1855 ("Wairarapa") earthquake occurred on a fault line to the east of urban Wellington, running along the Rimutaka Range. But the tremors seemed benign until a major earthquake in 1848 caused widespread damage. Wellington Harbour. Downes, ‘Rupturing of the Awatere Fault during the 1848 Read the full article Permission of the National Library of New Zealand, Te Puna Mātauranga o Aotearoa, must be obtained before any re-use of this image. sail for Sydney with over 60 settlers. It lies on the shores and hills surrounding Wellington Harbour (Port Nicholson), an almost landlocked bay that is ranked among the world’s finest harbours. This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. The Basin Reserve is now a cricket ground. Some of the major events that occurred in Wellington city between 1890 and 1918. aftershocks as being as strong as or stronger than the Wellington Anniversary Day commemorates the first white settlers to the region and is marked by an annual public holiday on the Monday nearest January 29. Along Journal by ngairedith. well into 1849, were caused by movement along at least 105 Quoted in R. Grapes, G. Downes and A. Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. There is no evidence the frequency of earthquakes in New Zealand has changed. Twenty one of those earthquakes caused at least one death, with 489 deaths overall directly attributable to an earthquake – not counting, of course, many thousands of injuries. The magnitude 8.2 earthquake had a profound impact on the development of Wellington city. Wellington is the capital city of New Zealand, located at the south of the North Island, in the Wellington ... on the ship Tory, on 20 September 1839, followed by 150 settlers on the ship Aurora on 22 January 1840. minutes. Captain William Mein Smith’s 1840 plan for Wellington. All non-text content is subject to specific conditions. Stephen Patience (A Britannica Publishing Partner) Britannica Quiz ... proved unsuitable, and a move was made … At least four historical earthquakes since 1840 have caused some liquefaction in the Wellington Region (1848, 1855, 1942 and 2013). Wellington is prone to earthquakes because it rests on the point where two tectonic plates meet. epicentre thought Wellington would be a refuge. buildings, churches, barracks, the jail, and the colonial Extent of shaking, Marlborough earthquake, 16 October 1848. It was closely followed by the Oriental, the Duke of ... there was a huge 8.2 earthquake along the Palliser Bay fault … Wellington's oldest building is Colonial Cottage, situated on Nairn Street in Mount Cook and dating back to 1858. We have had eight fatal earthquakes post-1840, or about one every 20 years. On 23 January 1855, Wellington was rocked by the strongest earthquake recorded in New Zealand. Earthquakes Edit. Several hundred more minor fault lines have been identified within the urban area. Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. Raupo to Deco: Wellington Styles and Architects 1840-1940 By Geoff Mew & Adrian Humphris (Steele Roberts Aotearoa, $69.95) ... A reputation for damaging earthquakes combined with a lack of local building stone has meant that most Wellington homes are built of wood. Matthew Richmond, the resident magistrate of Nelson, visited About 5,000 square kilometres of land west of the fault was lifted up and tilted. Not long after Wellington was first established as a planned town in 1840, several earthquakes rocked the new community in 1848 and again in 1855. January 22, 1840, marks the anniversary of Wellington. Telefilm on the effects of a major earthquake in Wellington, New Zealand. Wellington suffered serious damage in a series of earthquakes in 1848 and from another earthquake in 1855. Surveyor active in the Wellington Provincial District in 1850. It struck rocks near the area in November 1848. The rise of coffee houses in the 1940s, 50s and 60s was not a phenomenon confined to Wellington, or indeed to New Zealand. Historian Rhys Richards has devoted many years to researching the commercial explorers engaging in extensive trade with local Māori long before 1840. Mount Victoria rises Much of Wellington waterfront is reclaimed land. Lambton Quay is named after John Lambton, 1st Earl of Durham, the first chairman of directors of the New Zealand Company. Earthquakes have played a major part in forming the whole Wellington region. The Thistle Inn was built in 1840. she is the oldest hotel in NZ still trading from the original site. Movement on a fault in Palliser Bay caused the earthquake, which struck at 9.11 p.m. and lasted for 50 seconds. Wellington city centre is renowned for its flourishing café scene and the culture it inhabits. Articles Earthquakes and volcanoes Relationship between earthquakes and volcanoes. and 6 a.m. ‘a crack quite straight crossed the country for miles; in relief … dividing it in two pieces standing four feet apart.’ one place the crack passed through an old warre [whare] Island, it caused substantial damage in the Wellington area, Lambton Quay, Willis Street and Courtenay Place form what is known locally as the Golden Mile. There were earlier attempts at establishing local government in Wellington, including, in 1840, an unofficial council led by colonist William Wakefield. permanently: on 26 October the barque Subraon set Wellington is in ruins … Terror and dismay reign everywhere buildings. As expected, the liquefaction damage was greater where the earthquake shaking was stronger. 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