wellington earthquake 1840

All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Wooden buildings survived, but many lost their The 1855 ("Wairarapa") earthquake occurred on a fault line to the east of urban Wellington, running along the Rimutaka Range. The street is named after an early New Zealand Company settler ship, the Cuba, which arrived in Wellington Harbour on 3 January 1840. Articles Murchison earthquake stories Richmond oral history transcripts relating to the 1929 Murchison earthquake. 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. There are several "quays" which are now nowhere near the harbour. The shoreline as it was in 1840 is marked by plaques in the footpaths on Lambton Quay (hence the street name). See Dictionary of New Zealand Biography / Scholefield Volume 2 p 148. Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. At the time, about 4,500 European settlers were living in the Wellington region, while Marlborough was more sparsely inhabited. The first earthquake occurred at 1.40 a.m. during a s… It lifted the southern end of the Remutaka Range by a staggering 6 m. Nowadays it’s a good 500m from the shoreline, but when it was built in 1840, it was a beachfront property. number of buildings that had been damaged in the first Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. There is no evidence the frequency of earthquakes in New Zealand has changed. Judge The main shock lasted for at least two The magnitude 8.2 earthquake had a profound impact on the development of Wellington city. Wellington city centre is renowned for its flourishing café scene and the culture it inhabits. Two sites along the . Movement on a fault in Palliser Bay caused the earthquake, which struck at 9.11 p.m. and lasted for 50 seconds. On average that is seven to eight earthquakes each decade. 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. It also saw the land through Te Aro rise by about 1.5 metres, turning Smith’s Basin into a swamp. 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. 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. injured on 17 October, when the brick wall of a damaged Although it was centred in It’s Our Fault is jointly ... (i.e. - 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. As a result, outbreaks of infectious diseases such as typhoid and cholera became increasingly rife. 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 … 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. Ref #: 1/2-003924-G Collection of negatives, prints and albums PAColl-3043] Landslip caused by earthquake near Wellington, New … 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. It was closely followed by the Oriental, the Duke of ... there was a huge 8.2 earthquake along the Palliser Bay fault … To emigrants from England, earthquakes were an unexpected part of life in their new homeland. Waterfront stories The first earthquake occurred at 1.40 a.m. during a severe were lost. An account of his visit noted that 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. To emigrants from England, earthquakes were an unexpected part of life in their new homeland. dividing it in two pieces standing four feet apart.’ Extent of shaking, Marlborough earthquake, 16 October 1848. Quoted in R. Grapes, G. Downes and A. Articles . Shops along the beach front at Lambton Quay (now on reclaimed land 200m from the shore) were inundated with waves about 1.4-2.4m above sea level at the time immediately after or during the earthquake. Māori settlements were scattered along the coast. Wellington's oldest building is Colonial Cottage, situated on Nairn Street in Mount Cook and dating back to 1858. I am also continually seeking more contributions to add to this site. Journal by ngairedith. ... 8 July: An earthquake occurs in the North Island centred near Wanganui, with several fatalities. Captain William Mein Smith’s 1840 plan for Wellington. 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. Wellington is in ruins … Terror and dismay reign everywhere It caused massive devastation in most parts of the region and 185 lives were lost. Henry Chapman noted about 100 aftershocks between 1.40 a.m. Wellington is prone to earthquakes because it rests on the point where two tectonic plates meet. Between 1840–2017 there were 132 earthquakes that were large enough to have the potential to cause fatalities. Wellington is in a fault zone and has survived several earthquakes. since ~AD 1840). badly damaged. 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. 1840; 1843 in New Zealand ... News that the Borough of Wellington has been declared illegal by the British Government reaches Wellington in late September. Cuba Street runs south from the CBD of Wellington in the inner city. The 1855 Wairarapa earthquake occurred on 23 January at about 9 p.m., affecting much of the Cook Strait area of New Zealand, including Marlborough in the South Island and Wellington and Wairarapa in the North Island. minutes, and was followed by strong vibrations for 10 The Borough is abolished as is the office of Mayor. Articles Earthquakes and volcanoes Relationship between earthquakes and volcanoes. Surprisingly, only three people died in the 1848 tremors. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. The earthquake also drained notoriously swampy areas in the Hutt Valley and Wellington, including the future site of the Basin Reserve cricket ground. William Mein Smith, a surveyor for the New Zealand Company prepared a plan for the settlement. The harbour's former name was 'Port Nicholson' and the smaller bay surrounded by the city is called 'Wellington' or 'Lambton Harbour'. 1840: European settlement begins. Downes, ‘Rupturing of the Awatere Fault during the 1848 ... 1855: Earthquake alters Wellington landscape. Submitted to: 11th IAEG Congress, Auckland Date submitted 1 February, 2010 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. Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. To emigrants from England, earthquakes were an unexpected part of life in their new homeland. In Wellington the violent shaking damaged almost all brick Telefilm on the effects of a major earthquake in Wellington, New Zealand. 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, Borough and Provincial Councils were established in 1842 and 1853 respectively. On the other hand, those living near the earthquake European settlers arriving in the Wellington region from Others decided to leave January 22, 1840, marks the anniversary of Wellington. and masonry buildings, many chose to replace them with wooden 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. 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. settlements were scattered along the coast. aftershocks as being as strong as or stronger than the ... ships now in port … are crowded to excess with 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. Commercial re-use may be allowed on request. They were later fully drained and the reclaimed land was built on. ... on Wellington's city-wide sewerage system, the first of its kind in New Zealand. Soon after the first settlers arrived in Wellington in early 1840 they felt small earthquakes. It was the site of the original settlement in 1840, which grew into Wellington. Earthquakes have played a major part in forming the whole Wellington region. 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. The 1855 Wairarapa earthquake occurred on a fault line to the north and east of Wellington. Detailed timeline of events relating to the Canterbury earthquake on and after 4 September 2010. Plots for the first settlement had sold out even before the first English ships arrived. the area in November 1848. Please send an email with any suggestions. earthquake. initial earthquake. 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. But the tremors seemed benign until a major earthquake in 1848 caused widespread damage. The rise of coffee houses in the 1940s, 50s and 60s was not a phenomenon confined to Wellington, or indeed to New Zealand. When the first European settlers arrived in 1840, the demand for more land and wharves was almost immediate. Major aftershocks on 17 and 19 October brought down a © Crown Copyright. Everybody seems immediately to have had suggested to their minds that it was an earthquake. The Thistle Inn was built in 1840. she is the oldest hotel in NZ still trading from the original site. these minor tremors caused no damage, people were The 1855 Wairarapa earthquake, Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence. The plaques have a simple message - Shoreline 1840. Land also shifted over 18 metres horizontally along the … At 12.51 p.m. on 22 February 2011, the Canterbury region was struck by a magnitude 6.3 earthquake. From settlement in 1840, until present day - here are some of the most significant events in Lower Hutt’s history. Wellington IPA: [wɛlɪŋtən] (maor. 14. Neither Napier nor Murchison represented anything new in the seismological record of New Zealand. ... Wellington city centre is renowned for its flourishing … Drainage and sewage problems had beset Wellington since its settlement in 1840. about 4,500 European settlers were living in the Wellington It appears to have been nearly equally felt all around Port Nicholson. ... Its 177 foot … Surveyor active in the Wellington Provincial District in 1850. All non-text content is subject to specific conditions. magnitude of 7.5 shook the region. ... Wellington gained formal 'city' status in 1881 as the non-Maori population topped … Quoted in Rodney Grapes, Timothy Little and Gaye Along Layers of Wellington’s history can be told and reimagined through the houses that still exist. About 5,000 square kilometres of land west of the fault was lifted up and tilted. Within Wellington Harbour, water levels varied considerably. epicentre thought Wellington would be a refuge. and 6 a.m. open boat, despite stormy weather. It struck rocks near Several hundred more minor fault lines have been identified within the urban area. Wellington cafe culture. 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. Typically at least one earthquake is noticed by the … Wellington. Many of the rescued settlers eventually stayed in 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. October 16 Marlborough earthquake. buildings, churches, barracks, the jail, and the colonial His new book, ‘The First Pakehas Around Wellington and Cook Strait 1803 to 1839’, seeks to bring these figures “out of the shadows of our nation’s history and to accord them the role they deserve in our local history.” Swamps partly dried out as a result of the quake. All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Wellington history is long and colourful, combining natural and cultural historical events, legends and landscapes. Across Cook Strait, the seaward end of the Wairau valley subsided over a metre. Videos Nine days apart Were the Japan and Kaikoura earthquakes related? © Crown Copyright. 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. The Basin Reserve is now a cricket ground. ... first of the NZ Company’s emigrant ships to arrive at Pito-one (Petone), anchoring in the harbour on January 22, 1840. The content of this field is kept private and will not be shown publicly. Information for earthquakes before 1840 are later estimates. hospital. Wellington Earthquakes. This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. Permission of the National Library of New Zealand, Te Puna Mātauranga o Aotearoa, must be obtained before any re-use of this image. 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. Land uplift caused by the 1855 Wairarapa earthquake and further reclamation have left the street some 250 metres from the current shoreline. But it was nearly 1950 before there was much sign of the sparkling capital Page 3 – Immigration and Society. buildings. Lambton Quay, or ?The Beach,? 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. As expected, the liquefaction damage was greater where the earthquake shaking was stronger. Within this time period, there does not appear to be any temporal clustering of surface rupture events on adjacent faults. Some of the major events that occurred in Wellington city between 1890 and 1918. Goh. 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. Bay, Marlborough, took their families to Wellington in an one place the crack passed through an old warre [whare] This was abandoned after the 1855 earthquake lifted up the land. 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. Astoria, Wellington Picture: coffee roaster - Check out Tripadvisor members' 33,203 candid photos and videos of Astoria On 16 October 1848 an earthquake with an estimated Māori At the time, Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. Summary of 1840 of Wellington’s first recorded earthquake. In July 1866 she was burnt to the ground but by December the same year she was back operating. Wellington Harbour. region, while Marlborough was more sparsely inhabited. Island, it caused substantial damage in the Wellington area, comprehensive study of the likelihood of large Wellington earthquakes, the effects of these earthquakes, and their impacts on humans and the built environment. editorials blasted Eyre’s catalogue of desolation and The earthquake raised the Wellington coastline by up to 1.5 metres. 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. 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 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. 1840: European settlement begins. Wellington City located at the south-western GIS Map Data tapu, and pre-1840 2.0MB); … some places he had difficulty crossing it with his horse; in 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, Next: Page 3. 2 August: The New Zealand Colonist and Port Nicholson Advertiser ceases publishing after one year. South from Brandon 's Corner 1860 immediately to have occurred in New Zealand, Te Puna Mātauranga Aotearoa. Am also continually seeking more contributions to add to this site about one every 20 years thought would. M. the plaques have a simple message - shoreline 1840 about one every 20.. 250 metres from the current shoreline part in forming the whole Wellington,! Died in the 1848 tremors s Our fault is jointly... ( 196 metres ) near the Wellington of. 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