Images courtesy of Frontier Helicopters. The Edgecumbe Fault. The slip on the fault induces a difference in the phase registered by the satellite Orbit 1 Orbit 2 (after an earthquake) Phase A fissure up to 3 metres wide and 3–4 metres deep opened up along much of the fault, although some sections were marked just by zones of cracks. The M6.5 event was soon named after the town. 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. Kaikoura Earthquake and Tsunami: 14 November 2016 Post Event Report (National Emergency Management Agency response) Exercise Tangaroa post-exercise report. We’re continuing to work on improving the quality of our data, so please bear with us in the meantime. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. 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. Earthquake in Japan 11th March 2011. Earthquake Rubble. [2][3] It appears that the fault has ruptured at least once previously in the past 1800 years. They come from a collection of photographic albums covering disasters, exercises, course photographs, publicity material, staff photographs, study trips, emergencies, and overseas visits. [8], The Rangitaiki Plains lie within the Taupo Volcanic Zone, which is widening. See earthquake stock video clips. If something is not clear or seems incorrect, don’t hesitate to contact us using the online enquiries form. 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 … [2] Railway tracks in the town were bent and buckled,[1] and an 80-tonne New Zealand Railways DC class locomotive toppled over. Browse 1987 edgecumbe earthquake pictures, photos, images, GIFs, and videos on Photobucket Minutes later a much stronger quake rocked the region. The hypocentre was at a shallow depth of 8 km. 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 21:07 UTC: First to report: GEONET (NZ) after 2 minutes. 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. 55 54 10. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … A fissure up to 3 metres wide and 3–4 metres deep opened up along much of the fault, although some sections were marked just by zones of cracks. At 1:42pm on 2 March 1987 a large earthquake occurred in the northern Bay of Plenty, near the town of Edgecumbe. It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. In the Edgecumbe rail yards an 80-tonne locomotive lies on its side. There were indications that the first rupture propagated towards the south-west, triggering a second rupture 9 kilometres to the south-west and three seconds after the first. Date: 2nd march 1987 Magnitude: 6.5 Depth: 8 kilometers Death toll: … Edgecumbe Earthquake key vitals key vitals Total cost to rebuild the city and bring the community together : The cost all added up was about $300 million to fix all the damage caused. 109 82 19. 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