The 8.2 magnitude quake was centred 25 kilometres from the city - it was felt as far away as Canterbury in the South Island. Within Wellington harbour and on rivers and lakes in the region there may also be a ‘seiche’, as was observed in the harbour after the 1855 Wairarapa earthquake. 8 earthquakes within a radius of 150km of central Wellington over 24 hours Latest earthquake is #56458 being magnitude 2.26 ( II ) at 12.00 km at 5:23pm , about 4 hr 50 mins ago . In an early version of the manuscript, the main character, Florence, experiences the 1855 earthquake and its aftermath. 1855 earthquake Moon over Paekakariki Hill. 2015. iv The 1855 Wairarapa Earthquake Symposium Friday 9 September (Soundings Theatre, Level 2) Topic Speaker Organisation Start Duration Impact on humans and the built environment Humans The 1855 earthquake: societal impact and response in Wellington Hamish Campbell GNS 0840 20 Individuals' response to natural hazard events John McClure Victoria M 8.2 Wairarapa Tue, Jan 23 1855 The 1855 earthquake is the most severe earthquake to have occurred in New Zealand since systematic European colonisation began in 1840. The “Basin Reserve” sports ground in central Wellington is a well-known and unavoidable landmark, as a convergence point for four major roads which circle around its perimeter, as well as for fans of “the gentile sport”. 36 relations. From his observations it was deduced these seiche waves had and amplitude of 3 metres and a period of approximately 20 minutes (every 20 minutes the waves breached the shoreline) (Abraham 1997). The largest on record – but certainly not the largest ever – was the magnitude 8.2 Wairarapa earthquake of 1855. This earthquake was situated along the Wairarapa Fault and because of this it caused more faulting and uplift in the area situated around Wellington. 1855: Earthquake alters Wellington landscape. In this letter to a friend, Wellington merchant and Jewish congregation leader Abraham Hort gives a graphic description of the massive earthquake that struck Wairarapa and Wellington in January 1855. On August 16, 1868, a similar It is a peculiar fact that the tides are neaps at present. * In the water 27 km south-west of Ratana, New Zealand Napier was struck by an M 7.8 quake in 1931 and Kaikoura by an M 7.8 quake in 2016. It appears that almost all the buildings were made of wood. A seiche occurs when seismic waves passing through the water body set up standing waves that can then inundate the surrounding shorelines. In 1855 Wellington had only been settled for 15 years and was a relatively young, but busy, town. The jetties have been built further out to sea so that ships could be unloaded. The earthquake epicentres were both near Masterton, but the August quake was much deeper and thus less severe. The canyon starts just 10 kilometres off Wellington's coast and plunges to depths of 3km south of Cape Palliser. The next stranded beach, another metres higher, seems to have been uplifted about 2850 BCE (4800 BP), with an even earlier uplift of 7 metres in about 4850 BCE (6800 BP). buildings or infrastructure) About 10 minutes after the first shock, a tsunami swept the coast on both sides of Cook Strait. In-text: ([Gold, Charles Emilius] 1809-1871 :Landslip caused by earthquake near Wellington N. Zealand Jan 1855 | National Library of New Zealand, 2015) Your Bibliography: Natlib.govt.nz. Intensity of the earthquake The evening of 23 January 1855 was the end of a two-day holiday, the 15th anniversary of Wellington’s founding. This 1860 photograph looks south along Wellington’s Lambton Quay, with the uplifted 1855 beach. On January 23 rd 1855, an 8.2 magnitude earthquake st ruck Wairarapa in New Zealand’s North Island. This view of Wellington, drawn about 1852, shows the town as it developed after the 1848 earthquake.

NZ, had been placed on high alert about the possibility of tsunami wave and

Maori gath­ered the unexpected harvest for the next two days until putrefaction set in. Wellington, Central North Island earthquake: 5.8 magnitude quake near Levin shakes North Island 24 May, 2020 10:13 PM 9 minutes to read 5.8 magnitude earthquake near Levin shakes North Island. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. 1863 HMS Orpheus shipwreck After that the landscape had changed significantly. The earthquake caused widespread damage in Wellington. 1855 Wairarapa earthquake On 23 January a magnitude 8.2 earthquake struck the lower North Island. Recognizing the potential seismic hazard, the city has adopted building codes that maximize structural resistance to earthquake damage. 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. The Moral Compass is set predominantly in Wellington in 1853/4. This earthquake cause waves the height of 2 to 3.5 m to hit the Wellington harbour heads (Dawe et al. Though the 1855 earthquake was the most dramatic earthquake ever recorded in Wellington, many larger (and smaller) quakes have had a role in shaping our geography, our building practices, the lay-out of our city, and our social history. The 8.2 earthquake was massive, heaving the whole region like a quilt being shaken. Much of current downtown Wellington, as well as State Highway 2 from Wellington to the Hutt Valley, became useable real estate only after it was uplifted in that jolt. wellington earthquake 1855 death toll. The 1855 Wairarapa earthquake occurred on the Wairarapa Fault to the north and east of Wellington. To date it was the 2nd most powerful ever recorded in New Zealand only 4 people were killed. Modified Mercalli scale. In New Zealand's biggest historic 'quake in 1855, The Wairarapa Fault moved about 15 metres sideways and about 6 metres vertically! October 16, 2020 Uncategorized. running to and fro in all parts of the town. ... and may have been caused by the magnitude 8.2 Wairarapa earthquake in 1855." The earthquake was 8.6 in magnitude and due to the earthquake it made a massive landslide. A maximum of 100 earthquakes are displayed. The second to lowest (i.e. New Zealand’s largest ever earthquake was the magnitude 8.2–8.3 quake that struck on 23 January 1855. As a result of this great earthquake, the whole Wellington region was severely shaken, uplifted and tilted to the west. Earthquakes from the last 365 days that may have caused shaking Weak or greater in New Zealand. It was the end of a holiday weekend celebrating this milestone and most people were at home relaxing. 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