It's a tool, resource or reference for study, research, education, learning or teaching, that can be used by teachers, educators, pupils or students; The 1848 Marlborough earthquake was a 7.5 earthquake that occurred at 1:40 a.m. on 16 October 1848 and whose epicenter was in the Marlborough region of the South Island of New Zealand. On average, the country experiences about 15,000 earthquakes per year, but only around 250 of those events are large enough to be felt. The AIR Earthquake Model for New Zealand provides the most up-to-date and comprehensive view of earthquake risk and enables stakeholders to prepare for and mitigate potential future impacts. Extent of shaking, Wairarapa earthquake, 23 January 1855 Next. This earthquake was associated with the largest observed movement on a strike-slip fault, maximum 18 m. It has been suggested that the surface rupture formed by this event helped influence Charles Lyell to link earthquakes with rapid movement on faults. | Trademarks. severe earthquakes felt in the province of Wellington, List of New Zealand urban areas by population, List of international cricket five-wicket hauls at the Riverside Ground. It gives a brief definition of each concept and its relationships. AIR Worldwide | All rights reserved. The 2014 Eketahuna earthquake struck at 3:52 pm on 20 January, centred 15 km east of Eketahuna on the south-east of New Zealand's North Island. Dans l'île du Sud la majeure partie du déplacement relatif entre ces plaques est repris le long d' une seule dextre (latéral droit) décrochement avec une grande inverse composante, la faille Alpine . New Zealand lies along the boundary between the Australian and Pacific Plates. It shows the intensity of shaking during the earthquake of 23 January 1855. Tremors continued almost continuously until midnight and sporadic strong aftershocks were felt for several days. It has been suggested that the surface rupture formed by this event helped influence Charles Lyell to link earthquakes with rapid movement on faults. for the academic world: for school, primary, secondary, high school, middle, technical degree, college, university, undergraduate, master's or doctoral degrees; Unionpedia is a concept map or semantic network organized like an encyclopedia – dictionary. The last major earthquake on the Alpine Fault was in c. 1717 AD, the probability of another one occurring within the next 50 years is estimated at about 30 percent. The first shoreline inland from the present day coast is where the shoreline was in 1855, before the area was uplifted by the Wairarapa earthquake. Originally reported as magnitude 6.6 on the Richter Scale, the earthquake was later downgraded to a magnitude of 6.2. The Modified Mercalli scale (from 1 to 12) measures earthquakes by the intensity of shaking observed. Google Play, Android and the Google Play logo are trademarks of Google Inc. National Institute of Water and Atmospheric Research, 1855 Wairarapa earthquake and Alpine Fault, 1855 Wairarapa earthquake and Charles Lyell, 1855 Wairarapa earthquake and Christchurch, 1855 Wairarapa earthquake and Convergent boundary, 1855 Wairarapa earthquake and Cook Strait, 1855 Wairarapa earthquake and Fault (geology), 1855 Wairarapa earthquake and Geomorphology, 1855 Wairarapa earthquake and Indo-Australian Plate, 1855 Wairarapa earthquake and Kermadec Trench, 1855 Wairarapa earthquake and List of earthquakes in New Zealand, 1855 Wairarapa earthquake and List of historical earthquakes, 1855 Wairarapa earthquake and List of historical tsunamis, 1855 Wairarapa earthquake and Lyttelton, New Zealand, 1855 Wairarapa earthquake and Marlborough Fault System, 1855 Wairarapa earthquake and Marlborough Region, 1855 Wairarapa earthquake and Moment magnitude scale, 1855 Wairarapa earthquake and National Institute of Water and Atmospheric Research, 1855 Wairarapa earthquake and New Zealand, 1855 Wairarapa earthquake and North Island, 1855 Wairarapa earthquake and North Island Fault System, 1855 Wairarapa earthquake and Pacific Plate, 1855 Wairarapa earthquake and Rimutaka Range, 1855 Wairarapa earthquake and South Island, 1855 Wairarapa earthquake and Transform fault, 1855 Wairarapa earthquake and Turakirae Head, 1855 Wairarapa earthquake and Wairarapa Fault, 1855 Wairarapa earthquake and Wellington Harbour, 1855 Wairarapa earthquake and 1843 Wanganui earthquake, 1855 Wairarapa earthquake and 1848 Marlborough earthquake, 1855 Wairarapa earthquake and 1888 North Canterbury earthquake, https://en.wikipedia.org/wiki/1855_Wairarapa_earthquake, Creative Commons Attribution-ShareAlike License. The number of people killed is uncertain, but is estimated to be between five and nine. 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 epicentre was approximately 35 kilometres (22 mi) west of Hanmer. It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique convergent boundary between the Indo-Australian Plate and Pacific Plate, from the transform Alpine Fault to the Hikurangi Trench subduction zone. A total of 1112 aftershocks were recorded, ranging between magnitudes 2.0 and 4.9 on the Richter Scale. The … People fled outdoors, where they remained for the night in tents and makeshift beds, as incessant aftershocks rocked the area – one person counted 250 in the first 11 hours. Le tremblement de terre a généré le plus grand tsunami historique de Nouvelle-Zélande généré localement , avec une montée maximale de 10 à 11 m (33 à 36 pieds). The Wairarapa Fault is an active seismic fault in the southern part of the North Island of New Zealand. Wairarapa earthquake, 1855. The Alpine Fault is a geological fault that runs almost the entire length of New Zealand's South Island and forms the boundary between the Pacific Plate and the Indo-Australian Plate.