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[1] The hardest hit was Edgecumbe, with damage to approximately 50% of its houses. 130,711 earthquake stock photos, vectors, and illustrations are available royalty-free. The land on the north-western side dropped by up to 2.1 metres (6.9 ft),[7] and that area is now more prone to flooding. ... sergeant of the marines on James Cook's Endeavour expedition. 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. Sign in Sign up for FREE Prices and download plans Mt. 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. Toppled by the shaking. The region which sank downward is now more prone to flooding. [7] The old scarp had previously been unrecognised, but was later seen in aerial photographs taken before the earthquake. These northeast trending tectonic ruptures are widely distributed across the Edgecumbe is known to seismologists because fault lines which cross the North Island emerge at Edgecumbe, in the Eastern Bay of Plenty. The earthquake was the most damaging New Zealand had experienced in recent decades, with approximately 50% of the houses in Edgecumbe being damaged and 35 people being seriously injured. The Edgecumbe Fault. [1] The hypocentre was at a shallow depth of 8 km. This survey helped gain an understanding of the shear wave propagation characteristics across an active fault in the sediments of the area. 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. The people standing nearby show the scale of the rupture. 205 Free images of Earthquake. Wellington Earthquake National Initial Response Plan version 1.1 now available Results of the Disaster Preparedness Survey for 2017 now available [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. Images and media for edgecumbe. This Television New Zealand news coverage of 2 March 1987 reports the aftermath of the Edgecumbe earthquake. 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. [8], The Rangitaiki Plains lie within the Taupo Volcanic Zone, which is widening. We’re continuing to work on improving the quality of our data, so please bear with us in the meantime. Earthquake Rubble. Edgecumbe was the nearest centre to the magnitude 6.3 earthquake of 1987. Site Quicklinks Culture & Society. The largest rupture, the Edgecumbe Fault, was 7 kilometres (4.3 mi) long and formed on, and extended, a late Holocene fault scarp. 70 81 15. If something is not clear or seems incorrect, don’t hesitate to contact us using the online enquiries form. Brick Brickwork Ruin. Download all photos and use them even for commercial projects. [2], Twenty-five people suffered injuries that needed medical attention, but no-one was killed. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … 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 … Find the best free stock images about earthquake. Multiple massive earthquake hit Japan on 11th of March 2011. 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. [7] The intense ground shaking led to a large number of ground surface failures, including sand boils, ridge-top shatters and debris avalanches on steeper slopes. Buckled railway line and a locomotive flung on its side by the force of the Edgecumbe earthquake. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … 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. [3][4] Then there was a 5.2 ML earthquake at 1:35 pm on 2 March, followed by the main shock seven minutes later. Surface rupture produced by the 2010 Edgecumbe earthquake (New Zealand) Cumulated earthquakes produce topography . Jan 9, 2013 - Original Evening Post caption reads: "Graves lie broken and disturbed by fissures in the Kokohinau Marae cemetery, between Edgecumbe and Te Teko." Lava Cracked Background. [3][5] The main shock appears to have actually consisted of two ruptures, and possibly a third. ... Damage to the wall foundations during the 1987 earthquake may have also been a contributing factor. Archives Reference: ABUG W5083 7881 Box 12/ P87/3, archway.archives.govt.nz/ViewFullItem.do?code=1272861, For updates on our On This Day series and news from Archives New Zealand, follow us on Twitter twitter.com/ArchivesNZ, Caption information from www.teara.govt.nz/en/historic-earthquakes/page-11, www.teara.govt.nz/en/historic-earthquakes/page-11. [2] The most spectacular feature of the scarp was a deep prominent fissure up to 3 metres wide and 3–4 metres deep, mostly with near-vertical walls, that opened up along the fault. 4 Jan 21:07 UTC: First to report: GEONET (NZ) after 2 minutes. Earthquake Rubble. The San Andreas fault: cumulated ... images . Long-period body-wave modelling of the main shock of the 1987 March 2 Edgecumbe earthquake sequence reveals a multiple rupture event with a moment of 4. Kaikoura Earthquake and Tsunami: 14 November 2016 Post Event Report (National Emergency Management Agency response) Exercise Tangaroa post-exercise report. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. At 1:42pm on 2 March 1987 a large earthquake occurred in the northern Bay of Plenty, near the town of Edgecumbe. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. After the first earthquake the engine driver had climbed aboard to use the radio-telephone in the cab to warn other trains to stop. No one was killed, but several dozen people suffered serious injuries. 55 54 10. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. Bay of Plenty Earthquake, 1987 (16552659081).jpg 3,734 × 2,511; 2.04 MB It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. There was extensive damage to its milk factory, with large storage tanks toppled. [3][5], Eleven ground-surface ruptures occurred in the Rangitaiki Plains, though no active faults had previously been recognised on the Plains. An earthquake measuring 6.2 on the Richter scale struck Edgecumbe on 2nd March 1987. 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. The slip on the fault induces a difference in the phase registered by the satellite Orbit 1 Orbit 2 (after an earthquake) Phase Minutes later a much stronger quake rocked the region. Previous To … [1], "Historic earthquakes – The 1987 Edgecumbe earthquake", "Edgecombe [sic] earthquake: reconnaissance report", "1987 Edgecumbe Earthquake: 30 years ago today", Canterbury Earthquake Response and Recovery Act 2010, https://en.wikipedia.org/w/index.php?title=1987_Edgecumbe_earthquake&oldid=948461393, Creative Commons Attribution-ShareAlike License, This page was last edited on 1 April 2020, at 04:11. It was, with the exception of the Inangahua earthquake in 1968 , the most severe and damaging earthquake to hit New Zealand in 45 years. 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). In the Edgecumbe rail yards an 80-tonne locomotive lies on its side. Share this item Post to Pinterest Post to Facebook Post to Twitter. Edgecumbe Flood Information & Support. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. Related Images: disaster civil engineer collapse house rubble roads alley glimpse historical centre earthquake. 68 98 8. Browse 1987 edgecumbe earthquake pictures, photos, images, GIFs, and videos on Photobucket A DigitalNZ story by: David Clover - Images of the Edgecumbe earthquake 1987 Although not of an exceptional magnitude, it was damaging because it was very shallow. The first was off the coast of Miyagi, the second was of the The devastated Bay of Plenty town of Edgecumbe as photographed from the air. In a calibration survey the method was first tested over a surface trace of the Edgecumbe Fault 30 km south-west of Whakatane township, that ruptured during the 1987 Mw 6.3 Edgecumbe Earthquake. Hdr Destroyed Area. Images courtesy of Frontier Helicopters. [6] The largest aftershock measured 5.6 and struck nine minutes later at 1.51 pm. earthquake images. [2] Railway tracks in the town were bent and buckled,[1] and an 80-tonne New Zealand Railways DC class locomotive toppled over. 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. ... All images & media in this story. A selection of dramatic images from New Zealand earthquakes. 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. 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. Minutes later a much stronger quake rocked the region. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. The Edgecumbe earthquake was the first since the 1968 Īnangahua quake to cause major damage. 4 Jan 21:08: Magnitude recalculated from 2.1 to 2.0. The photographs were captured under clear bright blue skies in contrast to the water logged devastation below. There is also the possibility of a third, significantly smaller, rupture another ten seconds later. During the Edgecumbe earthquake, the area widened by 1.2 metres. Media in category "Edgecumbe earthquake (1987) at Archives New Zealand" The following 10 files are in this category, out of 10 total. The Pleistocene-to-Holocene Edgecumbe volcanic field covers about 260 km2 of Kruzov Island west of Sitka in the SE panhandle of Alaska. 400 445 52. The main rift created by the earthquake. The earthquake had been caused by movement along the fault; the land to the north-west had dropped by up to 2 metres. Earthquake in Japan 11th March 2011. Volcano Geography Views. 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. Abstract The Edgecumbe earthquake, 1987 March 2 (ML 6.3), was associated with renewed tectonic rupture on the Edgecumbe Fault, renewed movement on the Onepu and Rotoitipakau Faults, and several new surface breaks-the Awaiti, Otakiri, Te Teko, and OmeheuFaults. Edgecumbe Earthquake, N.Z., 1987 Edgecumbe Earthquake, N.Z., 1987; Filter By Type All Results 31. There is a group of men beside the tracks. The M6.5 event was soon named after the town. 109 82 19. 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