Site Quicklinks Culture & Society. [9], The most damage was in the towns of Edgecumbe, Te Teko, Kawerau, Matata and Thornton, where chimneys toppled and poorly constructed houses were seriously damaged. There is a group of men beside the tracks. 205 Free images of Earthquake. See earthquake stock video clips. At 1:42pm on 2 March 1987 a large earthquake occurred in the northern Bay of Plenty, near the town of Edgecumbe. The basaltic-to-dacitic field is dominated by the large composite cones of Mount Edgecumbe, Crater Ridge, and Shell Mountain, and has an unusual tectonic setting only 16 km E of the Queen Charlotte-Fairweather transform fault separating … The earthquake had been caused by movement along the fault; the land to the north-west had dropped by up to 2 metres. [1][2] The foreshock seven minutes before the main shock had cut the power supply, and many people had moved away from heavy machinery and out of buildings that then collapsed in the main earthquake. At 1.35 p.m. on 2 March 1987, a magnitude 5.2 earthquake struck the Bay of Plenty region, cutting power and sending many people outdoors. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, and smaller aftershocks were felt for weeks. During the Edgecumbe earthquake, the area widened by 1.2 metres. Steven A Christensen, Dept of Civil Engineering, University of Canterbury (EQC funded report 93/136) Abstract. Sign in Sign up for FREE Prices and download plans 400 445 52. Mt. [GNS Science] These railway lines, originally straight, were left buckled after the earthquake, distorted by the intense ground motion. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. As these images are from the Ministry of Civil Defence, Central Regional Office. It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. The 1987 Edgecumbe earthquake measured 6.5 on the moment magnitude scale and struck the Bay of Plenty region of New Zealand at 1:42 pm on 2 March. 4 Jan 21:10: Hypocenter depth recalculated from 5.4 to 4.6 km (from 3.4 to 2.9 mi).Epicenter location corrected by 1.4 km (0.9 mi) towards SE. Surface rupture produced by the 2010 Edgecumbe earthquake (New Zealand) Cumulated earthquakes produce topography . Edgecumbe War Memorial Hall. At 1.35 p.m. on 2 March 1987, a magnitude 5.2 earthquake struck the Bay of Plenty region, cutting power and sending many people outdoors. Edgecumbe Earthquake, N.Z., 1987 Edgecumbe Earthquake, N.Z., 1987; Filter By Type All Results 31. The epicentre was 2.24 kilometres (1.39 mi) south-south-east of the town of Matata, and 15 kilometres (9.3 mi) north-north-west of Edgecumbe, on the Rangitaiki Plains (the floodplain of the Rangitaiki River, the Tarawera River and the Whakatane River). After the first earthquake the engine driver had climbed aboard to use the radio-telephone in the cab to warn other trains to stop. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. Kaikoura Earthquake and Tsunami: 14 November 2016 Post Event Report (National Emergency Management Agency response) Exercise Tangaroa post-exercise report. This survey helped gain an understanding of the shear wave propagation characteristics across an active fault in the sediments of the area. A swarm started on 21 February off-shore from Maketu, near Te Puke, 40 kilometres from the main shock's epicentre, and another swarm started on 26 February between Matata and Thornton, very close to the epicentre. Earthquake in Japan 11th March 2011. [3] The northern end of the scarp is one kilometre east of Edgecumbe, and the scarp runs southwest to a point three kilometres north of Te Teko. 157 172 16. 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