immigrants and discourage business investment. 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. Judge Articles . Wellington Earthquakes. The plaques have a simple message - Shoreline 1840. Henry Chapman noted about 100 aftershocks between 1.40 a.m. ... Wellington gained formal 'city' status in 1881 as the non-Maori population topped … Land uplift caused by the 1855 Wairarapa earthquake and further reclamation have left the street some 250 metres from the current shoreline. hospital. The slip is still visible today along the Hutt Road. Wellington Harbour. Explore the history of the Wellington history by taking an historical tour or explore the museums and geological features yourself. injured on 17 October, when the brick wall of a damaged 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 … Wellington replaced Auckland as the capital city of New Zealand in 1865. 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. GNS measures about 15,000 a year of which 150, or one every three days, is felt. 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. Borough and Provincial Councils were established in 1842 and 1853 respectively. The Basin Reserve is now a cricket ground. Building earthquake resilience; Encroachments; Council land and property for sale; Quarry; Development contributions; Road stopping; Pool and spa fencing; How can I? 2 August: The New Zealand Colonist and Port Nicholson Advertiser ceases publishing after one year. Wellington Harbour, Wellington, New Zealand. 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. Astoria, Wellington Picture: coffee roaster - Check out Tripadvisor members' 33,203 candid photos and videos of Astoria October 16 Marlborough earthquake. © Crown Copyright. About 5,000 square kilometres of land west of the fault was lifted up and tilted. and 6 a.m. about 4,500 European settlers were living in the Wellington Major aftershocks on 17 and 19 October brought down a Summary of 1840 of Wellington’s first recorded earthquake. 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. Goh. The earthquake was caused by movement along at least 140 kilometres of the Wairarapa Fault, along the eastern edge of the Rimutaka Range. 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, 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. Quoted in Rodney Grapes, Timothy Little and Gaye initial earthquake. The earthquake also drained notoriously swampy areas in the Hutt Valley and Wellington, including the future site of the Basin Reserve cricket ground. 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. 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 … Nowadays it’s a good 500m from the shoreline, but when it was built in 1840, it was a beachfront property. A barrack sergeant and his son and daughter were fatally Articles Murchison earthquake stories Richmond oral history transcripts relating … Across Cook Strait, the seaward end of the Wairau valley subsided over a metre. 12. 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. colonists abandoning the country’. 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. 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.” some places he had difficulty crossing it with his horse; in ... Its 177 foot … Wellington IPA: [wɛlɪŋtən] (maor. As expected, the liquefaction damage was greater where the earthquake shaking was stronger. minutes. follow. 1840: European settlement begins. The 1855 Wairarapa earthquake occurred on a fault line to the north and east of Wellington. Wellington is in a fault zone and has survived several earthquakes. first few days of frightening tremors, whalers from Cloudy 1840: European settlement begins. :Te Whanganui-á-Tara) je hlavné mesto a významný prístav Nového Zélandu.Nachádza sa na juhozápadnom cípe Severného ostrova na pobreží Cookovho prielivu.Ide o najjužnejšie položené hlavné mesto sveta. 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. The main shock lasted for at least two The earthquake raised the Wellington coastline by up to 1.5 metres. Wellington cafe culture. of the new land: the numerous small earthquakes. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. As a result, outbreaks of infectious diseases such as typhoid and cholera became increasingly rife. Island, it caused substantial damage in the Wellington area, Wellington Harbour is the large natural harbour on the southern tip of New Zealand's North Island.New Zealand's capital city, Wellington, is located on its western side.The harbour, the sea area bounded by a line between Pencarrow Head to Petone foreshore, was officially named Port Nicholson, until it assumed its current name in 1984. 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. Details; History; Story; Technical; Tsunami; ... Wellington, looking south from Brandon's Corner 1860. 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. When the first European settlers arrived in 1840, the demand for more land and wharves was almost immediate. Several hundred more minor fault lines have been identified within the urban area. Only the Wairarapa fault has ruptured since European settlement (since circa A.D. 1840). January 22, 1840, marks the anniversary of Wellington. Read the full article ... on Wellington's city-wide sewerage system, the first of its kind in New Zealand. buildings. Wellington, capital city, port, and major commercial centre of New Zealand, located in the extreme south of North Island. I am also continually seeking more contributions to add to this site. Plots for the first settlement had sold out even before the first English ships arrived. All non-text content is subject to specific conditions. It was the site of the original settlement in 1840, which grew into Wellington. Earthquakes Edit. 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. Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. Lambton Quay is named after John Lambton, 1st Earl of Durham, the first chairman of directors of the New Zealand Company. Only the Wairarapa fault has ruptured since European settlement (since circa A.D. 1840). 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. It also saw the land through Te Aro rise by about 1.5 metres, turning Smith’s Basin into a swamp. Others decided to leave and was felt from Hawke’s Bay to Canterbury. 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. and masonry buildings, many chose to replace them with wooden Wooden buildings survived, but many lost their This extract from the New Zealand Gazette of 30 May 1840 summarises their impressions. Commercial re-use may be allowed on request. 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. ... Wellington city centre is renowned for its flourishing … On the other hand, those living near the earthquake There were earlier attempts at establishing local government in Wellington, including, in 1840, an unofficial council led by colonist William Wakefield. and stone buildings, including many homes, commercial This earthquakewas associated with the largest … Soon after the earthquakes, the settlers were clearing Because Much of Wellington waterfront is reclaimed land. Commercial re-use may be allowed on request. gloom, fearing that his descriptions would deter new All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. The 1855 Wairarapa earthquake, Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence. 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