Only the Wairarapa fault has ruptured since European settlement (since circa A.D. 1840). It was closely followed by the Oriental, the Duke of ... there was a huge 8.2 earthquake along the Palliser Bay fault … The first movement took place at about twenty minutes to five o’clock in the morning of the 26th May; the second about an hour later. number of buildings that had been damaged in the first Matthew Richmond, the resident magistrate of Nelson, visited Ref #: 1/2-003924-G Collection of negatives, prints and albums PAColl-3043] Landslip caused by earthquake near Wellington, New … It’s Our Fault is jointly ... (i.e. Journal by ngairedith. Wellington suffered serious damage in a series of earthquakes in 1848 and from another earthquake in 1855. European settlers arriving in the Wellington region from open boat, despite stormy weather. Several hundred more minor fault lines have been identified within the urban area. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. Articles Earthquakes and volcanoes Relationship between earthquakes and volcanoes. gloom, fearing that his descriptions would deter new one place the crack passed through an old warre [whare] Typically at least one earthquake is noticed by the … There is no evidence the frequency of earthquakes in New Zealand has changed. © Crown Copyright. There were earlier attempts at establishing local government in Wellington, including, in 1840, an unofficial council led by colonist William Wakefield. To emigrants from England, earthquakes were an unexpected part of life in their new homeland. 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. Wellington is prone to earthquakes because it rests on the point where two tectonic plates meet. 1 Angry newspaper Quoted in R. Grapes, G. Downes and A. night aboard ships in the harbour. Plots for the first settlement had sold out even before the first English ships arrived. Astoria, Wellington Picture: coffee roaster - Check out Tripadvisor members' 33,203 candid photos and videos of Astoria Submitted to: 11th IAEG Congress, Auckland Date submitted 1 February, 2010 Drainage and sewage problems had beset Wellington since its settlement in 1840. On the other hand, those living near the earthquake Goh. Wellington New Zealand history information and historical places. It caused massive devastation in most parts of the region and 185 lives were lost. Some of the major events that occurred in Wellington city between 1890 and 1918. The first earthquake occurred at 1.40 a.m. during a s… Along They were later fully drained and the reclaimed land was built on. Although it was centred in 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. ... Its 177 foot … William Mein Smith, a surveyor for the New Zealand Company prepared a plan for the settlement. Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. Summary of 1840 of Wellington’s first recorded earthquake. The earthquake was caused by movement along at least 140 kilometres of the Wairarapa Fault, along the eastern edge of the Rimutaka Range. Extent of shaking, Marlborough earthquake, 16 October 1848. ... ships now in port … are crowded to excess with kilometres of a major fault along the Awatere Valley. buildings. But it was nearly 1950 before there was much sign of the sparkling capital Page 3 – Immigration and Society. To emigrants from England, earthquakes were an unexpected part of life in their new homeland. 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. Explore the history of the Wellington history by taking an historical tour or explore the museums and geological features yourself. The harbour's former name was 'Port Nicholson' and the smaller bay surrounded by the city is called 'Wellington' or 'Lambton Harbour'. Welcome to the Wellington pages of the New Zealand GenWeb Project. colonists abandoning the country’. Earthquakes Edit. ruins and rebuilding. Wooden buildings survived, but many lost their … Wellington's oldest building is Colonial Cottage, situated on Nairn Street in Mount Cook and dating back to 1858. The basis of the modern-day waterfront area was shaped by changes that occurred in the 1970s - 1980s. Bay, Marlborough, took their families to Wellington in an Wellington is in ruins … Terror and dismay reign everywhere Articles Murchison earthquake stories Richmond oral history transcripts relating to the 1929 Murchison earthquake. Land uplift caused by the 1855 Wairarapa earthquake and further reclamation have left the street some 250 metres from the current shoreline. In 1893, the parliament in Wellington passed th e 'Electoral Act 1893' which made New Zealand the world's first country to give women the vote. Across Cook Strait, the seaward end of the Wairau valley subsided over a metre. There were earlier attempts at establishing local government in Wellington, including, in 1840, an unofficial council led by colonist William Wakefield. Services provided include passports, citizenship and birth, death and marriage registration, lottery and community grants, charities registration, gambling and censorship regulation, internet safety, antispam, local government, ethnic affairs, support services to the executive, and information and communication technology services for all of government. Mount Victoria rises Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. building collapsed during a major aftershock. Swamps partly dried out as a result of the quake. All non-text content is subject to specific conditions. The following night there was another slight shock, and since then there have been two more shocks, which have, however, been so slight, as to have been felt by a few. Many people in Wellington described these the 1848 earthquake in alarming terms: ‘the town of Wellington suffered serious damage in a series of earthquakes in 1848 and from another earthquake in 1855. 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. Wellington city centre is renowned for its flourishing café scene and the culture it inhabits. Mindful of the severe damage to brick Everybody seems immediately to have had suggested to their minds that it was an earthquake. Wellington (Māori: Te Whanganui-a-Tara [tɛ ˈfaŋanʉi a taɾa]) 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 major population centre of the southern North Island, and is the administrative centre of the Wellington Region, which also includes the Kapiti Coast and the Wairarapa.It is the … This was abandoned after the 1855 earthquake lifted up the land. Lieutenant Governor Edward Eyre described the effects of 1840: European settlement begins. This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. First record of a Wellington earthquake. LAMBTON QUAY, Wellington - 1840. The Wellington region is cut by five active right-lateral strike-slip faults: Wairarapa, Wellington, Ohariu, Shepherds Gully/Pukerua, and Wairau faults that have average recurrence intervals of meter-scale surface rupture that range from ̃500 years to 5000 years, and lateral slip rates that range from 1 to 10 mm/yr. The 8.2 magnitude quake was … ... Wellington city centre is renowned for its flourishing … ... 1855: Earthquake alters Wellington landscape. Since 1840, several major quakes have disrupted towns and cities, and caused injury and death..." Geonet — the 1855 Wairarapa earthquake "The 1855 earthquake is the most severe … Nowadays it’s a good 500m from the shoreline, but when it was built in 1840, it was a beachfront property. 1840; 1843 in New Zealand ... News that the Borough of Wellington has been declared illegal by the British Government reaches Wellington in late September. well into 1849, were caused by movement along at least 105 In July 1866 she was burnt to the ground but by December the same year she was back operating. Arrived in Wellington in 1840 as a surveyor with New Zealand Company. While it is true that two majors inside six years is unusual, we should treat the 40-year lull between Inangahua and Christchurch as unusually long. Cuba Street runs south from the CBD of Wellington in the inner city. Wellington history dates back as far as 950 AD according to Māori legend. Commercial re-use may be allowed on request. the area in November 1848. 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. Wellington is in a fault zone and has survived several earthquakes. Wellington. More recent history: the 1970s–1980s. sail for Sydney with over 60 settlers. The Basin Reserve is now a cricket ground. first few days of frightening tremors, whalers from Cloudy It appears to have been nearly equally felt all around Port Nicholson. Soon after the earthquakes, the settlers were clearing After the and stone buildings, including many homes, commercial At least four historical earthquakes since 1840 have caused some liquefaction in the Wellington Region (1848, 1855, 1942 and 2013). 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. This earthquakewas associated with the largest … initial earthquake. In it’s 180 years in business, the pub had seen some famed clientele. The plaques have a simple message - Shoreline 1840. were lost. When the first European settlers arrived in 1840, the demand for more land and wharves was almost immediate. All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Date Location Region … It lifted the southern end of the Remutaka Range by a staggering 6 m. ... on Wellington's city-wide sewerage system, the first of its kind in New Zealand. Māori Wellington Harbour, Wellington, New Zealand. Wellington Harbour before the Haowhenua earthquake, Extent of shaking, Marlborough earthquake, 16 October 1848, Eileen McSaveney, 'Historic earthquakes - The 1848 Marlborough earthquake', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/en/document/4379/first-record-of-a-wellington-earthquake (accessed 16 December 2020), Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 28 Mar 2011, updated 1 Nov 2017. To emigrants from England, earthquakes were an unexpected part of life in their new homeland. some places he had difficulty crossing it with his horse; in As a result, outbreaks of infectious diseases such as typhoid and cholera became increasingly rife. Two sites along the . the Awatere valley in the Marlborough district of the South It ranks as probably the most powerful earthquake in recorded New Zealand history, with an estimated magnitude of at least 8.2 on the Richter scale. Please send an email with any suggestions. January 22, 1840, marks the anniversary of Wellington. National Library of New Zealand, Papers Past Reference: follow. Earthquake casualties have been estimated for two situations, (i) scenario events on the Wellington Fault, and (ii) probabilistically, for all significant earthquake sources in New Zealand. The Borough is abolished as is the office of Mayor. 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. Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Historian Rhys Richards has devoted many years to researching the commercial explorers engaging in extensive trade with local Māori long before 1840. Wellington is prone to earthquakes because it rests on the point where two tectonic plates meet. At one end is the Michael Fowler Centre close to the harbour, and the other end is close to Aro Valley and at the base of the Mt Cook and Brooklyn hills. Detailed timeline of events relating to the Canterbury earthquake on and after 4 September 2010. The Thistle Inn was built in 1840. she is the oldest hotel in NZ still trading from the original site. In 1840 surveyors divided the peninsula into 18 lots, 5 of which were purchased by James Watt, who never lived there, and the name 'Watts Peninsula' was adopted. Island, it caused substantial damage in the Wellington area, 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. In Wellington the violent shaking damaged almost all brick 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. buildings, churches, barracks, the jail, and the colonial permanently: on 26 October the barque Subraon set region, while Marlborough was more sparsely inhabited. Astoria, Wellington Picture: coffee roaster - Check out Tripadvisor members' 33,172 candid photos and videos. It wa… It was the site of the original settlement in 1840, which grew into Wellington. Much of Wellington waterfront is reclaimed land. Read more... 26 February 1844 'Pistols at dawn': deadly duel in Wellington ... settlers at Port Nicholson (Wellington), where he served as the New Zealand Company’s Principal Agent between 1840 and 1848. 13. As one of the oldest suburbs in Aotearoa, with its streets laid out in 1840 by Mein Smith, 85% properties pre-date 1930,and are largely Victorian and Edwardian. dividing it in two pieces standing four feet apart.’ 14. of the new land: the numerous small earthquakes. Telefilm on the effects of a major earthquake in Wellington, New Zealand. 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. Wellington history is long and colourful, combining natural and cultural historical events, legends and landscapes. On 16 October 1848 an earthquake with an estimated magnitude of 7.5 shook the region. An account of his visit noted that This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. Articles Warships help in rescue response U.S., Canadian and Australian warships help Kaikoura after the earthquakes. Layers of Wellington’s history can be told and reimagined through the houses that still exist. Articles Murchison earthquake stories Richmond oral history transcripts relating … Among the effects of the earthquake was a new shoreline which increased the city’s footprint and made the Hutt Valley more accessible. The excitement of the fire had hardly ceased, when the Colonists were aroused by an undulatory motion of the earth, and a somewhat severe shaking of their houses. The 1929 Arthur’s Pass and Murchison earthquakes, The 2010 Canterbury (Darfield) earthquake, Personal stories of the 2010–11 Canterbury earthquakes, Personal stories of earthquakes since 1942, Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence. Only the Wairarapa fault has ruptured since European settlement (since circa A.D. 1840). The southern end of the Remutaka Range rose by over 6 metres, but the uplift decreased westward to near zero along the west coast of the Wellington peninsula. Articles . GNS measures about 15,000 a year of which 150, or one every three days, is felt. aftershocks as being as strong as or stronger than the The shoreline as it was in 1840 is marked by plaques in the footpaths on Lambton Quay (hence the street name). Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. From Ministry for Culture and Heritage: Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. From settlement in 1840, until present day - here are some of the most significant events in Lower Hutt’s history. The main shock lasted for at least two See Dictionary of New Zealand Biography / Scholefield Volume 2 p 148. the Wellington Harbour entrance and was wrecked, but no lives ill-prepared for the severity of the quakes that were to © Crown Copyright. Land uplift caused by the 1855 Wairarapa earthquake and further reclamation have left the street some 250 metres from the current shoreline. 2, Eileen McSaveney, 'Historic earthquakes - The 1848 Marlborough earthquake', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/en/historic-earthquakes/page-2 (accessed 16 December 2020), Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 28 Mar 2011, updated 1 Nov 2017. Originally an island called 'Motu-kairangi' until sometime after 1460 when a major earthquake joined it to the mainland, and the name 'Whataitai' was used. immigrants and discourage business investment. Vibrations continued for at least an hour, Images ... Summary of 1840 of Wellington’s first recorded earthquake. Videos Nine days apart Were the Japan and Kaikoura earthquakes related? and masonry buildings, many chose to replace them with wooden Large landslips had swept down the sides of the Rimutaka Ranges, and there were gaping fissures (cracks) in the Wairarapa Plain, some up to 5 metres deep. 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 magnitude 8.2 earthquake had a profound impact on the development of Wellington city. 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. 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. Lambton Quay is named after John Lambton, 1st Earl of Durham, the first chairman of directors of the New Zealand Company. Neither Napier nor Murchison represented anything new in the seismological record of New Zealand. On 23 January 1855, Wellington was rocked by the strongest earthquake recorded in New Zealand. The 1855 earthquake is the most severe earthquake to have occurred in New Zealand since systematic European colonisation began in 1840. As aftershocks continued, some people sought safety at At the time, Paleoseismological studies on these faults have allowed the compilation of a complete record of surface rupture events over the past ∼1000 years in the Wellington region. minutes. Much of Wellington waterfront is reclaimed land. [Denton, Frank J, 1869-1963. about 4,500 European settlers were living in the Wellington New Zealand Gazette, 30 May 1840, p. 2. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. 12. The first earthquake occurred at 1.40 a.m. during a severe The town then relocated to the south-western end of the harbour. Within Wellington Harbour, water levels varied considerably. Also worked on Hawkes Bay maps for Donald McLean, surveyed Ahuriri Block; in 1860 moved to Canterbury and member of Canterbury Provincial Government survey party contracted to lay-off a road to West … Major aftershocks on 17 and 19 October brought down a The main purpose of the this website is to bring together the genealogical resources of the Wellington area to help with your research. All non-text content is subject to specific conditions. 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, Between 1840–2017 there were 132 earthquakes that were large enough to have the potential to cause fatalities. Permission of the National Library of New Zealand, Te Puna Mātauranga o Aotearoa, must be obtained before any re-use of this image. injured on 17 October, when the brick wall of a damaged The 1848 earthquakes, and the aftershocks which continued It struck rocks near February 2011 Christchurch earthquake. ... 8 July: An earthquake occurs in the North Island centred near Wanganui, with several fatalities. Others decided to leave - 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. hospital. 1840: European settlement begins. Henry Chapman noted about 100 aftershocks between 1.40 a.m. The moment magnitude is estimated to have been in the range 8.2–8.3, the most powerful recorded in New Zealand since systematic European colonisation began in 1840. Obtained before any re-use of this image for its flourishing café scene and the reclaimed land was built in,... 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