Find the best free stock images about earthquake. Brick Brickwork Ruin. An earthquake measuring 6.2 on the Richter scale struck Edgecumbe on 2nd March 1987. At 1:42pm on 2 March 1987 a large earthquake occurred in the northern Bay of Plenty, near the town of Edgecumbe. 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. [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. The first was off the coast of Miyagi, the second was of the Earthquake Rubble. 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 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. Liquefaction of Cohesionless Soils in the March 2, 1987 Edgecumbe Earthquake, Bay of Plenty, New Zealand, and other Earthquakes. If it's safe to do so, send us your newstips, video and images to newstips@stuff.co.nz "Get and stay out," was the Government's advice to to the people of Edgecumbe… Edgecumbe earthquake On the afternoon of 2 March 1987, at 1:42pm, the Bay of Plenty region was rocked by a magnitude 6.3 earthquake. The M6.5 event was soon named after the town. Multiple massive earthquake hit Japan on 11th of March 2011. ... All images & media in this story. [2], Twenty-five people suffered injuries that needed medical attention, but no-one was killed. [3][5] The main shock appears to have actually consisted of two ruptures, and possibly a third. 4 Jan 21:07 UTC: First to report: GEONET (NZ) after 2 minutes. The devastated Bay of Plenty town of Edgecumbe as photographed from the air. The photographs were captured under clear bright blue skies in contrast to the water logged devastation below. The Edgecumbe earthquake was the first since the 1968 Īnangahua quake to cause major damage. After the first earthquake the engine driver had climbed aboard to use the radio-telephone in the cab to warn other trains to stop. Buckled railway line and a locomotive flung on its side by the force of the Edgecumbe earthquake. earthquake images. It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. 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. Surface rupture produced by the 2010 Edgecumbe earthquake (New Zealand) Cumulated earthquakes produce topography . During the Edgecumbe earthquake, the area widened by 1.2 metres. 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. 400 445 52. Images and media for edgecumbe. Edgecumbe Flood Information & Support. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. Mt. Located on Japonski Island, across Mount Edgecumbe may refer to: Mount Edgecumbe Alaska a dormant volcano located on Kruzof Island in Alaska, USA Putauaki or Mount Edgecumbe a volcanic Mount Edgecumbe is a dormant volcano located at the … 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. As these images are from the Ministry of Civil Defence, Central Regional Office. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. Share this item Post to Pinterest Post to Facebook Post to Twitter. 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). Previous To … Edgecumbe War Memorial Hall. Although not of an exceptional magnitude, it was damaging because it was very shallow. The hypocentre was at a shallow depth of 8 km. [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. Download all photos and use them even for commercial projects. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, and smaller aftershocks were felt for weeks. There was extensive damage to its milk factory, with large storage tanks toppled. The earthquake had been caused by movement along the fault; the land to the north-west had dropped by up to 2 metres. The region which sank downward is now more prone to flooding. No one was killed, but several dozen people suffered serious injuries. Edgecumbe is a small town of around 1800 people, 18km west of Whakatane. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. The Edgecumbe Fault. 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." There is a group of men beside the tracks. A selection of dramatic images from New Zealand earthquakes. 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 … Earthquake in Japan 11th March 2011. Edgecumbe is known to seismologists because fault lines which cross the North Island emerge at Edgecumbe, in the Eastern Bay of Plenty. 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. [1] The hypocentre was at a shallow depth of 8 km. 68 98 8. 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. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … [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. [6] The largest aftershock measured 5.6 and struck nine minutes later at 1.51 pm. Steven A Christensen, Dept of Civil Engineering, University of Canterbury (EQC funded report 93/136) Abstract. Toppled by the shaking. The slip on the fault induces a difference in the phase registered by the satellite Orbit 1 Orbit 2 (after an earthquake) Phase [7] The old scarp had previously been unrecognised, but was later seen in aerial photographs taken before the earthquake. [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. 55 54 10. [1] The hardest hit was Edgecumbe, with damage to approximately 50% of its houses. 70 81 15. They come from a collection of photographic albums covering disasters, exercises, course photographs, publicity material, staff photographs, study trips, emergencies, and overseas visits. The San Andreas fault: cumulated ... images . Minutes later a much stronger quake rocked the region. In the Edgecumbe rail yards an 80-tonne locomotive lies on its side. Minutes later a much stronger quake rocked the region. [2] Railway tracks in the town were bent and buckled,[1] and an 80-tonne New Zealand Railways DC class locomotive toppled over. ... Damage to the wall foundations during the 1987 earthquake may have also been a contributing factor. 109 82 19. It was, with the exception of the Inangahua earthquake in 1968 , the most severe and damaging earthquake to hit New Zealand in 45 years. If something is not clear or seems incorrect, don’t hesitate to contact us using the online enquiries form. Related Images: disaster civil engineer collapse house rubble roads alley glimpse historical centre earthquake. 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 … A DigitalNZ story by: David Clover - Images of the Edgecumbe earthquake 1987 Kaikoura Earthquake and Tsunami: 14 November 2016 Post Event Report (National Emergency Management Agency response) Exercise Tangaroa post-exercise report. Edgecumbe High School abbreviated MEHS is a public boarding high school in Sitka, Alaska in the United States. This Television New Zealand news coverage of 2 March 1987 reports the aftermath of the Edgecumbe earthquake. Edgecumbe Earthquake, N.Z., 1987 Edgecumbe Earthquake, N.Z., 1987; Filter By Type All Results 31. 4 Jan 21:08: Magnitude recalculated from 2.1 to 2.0. Media in category "Edgecumbe earthquake (1987) at Archives New Zealand" The following 10 files are in this category, out of 10 total. [GNS Science] These railway lines, originally straight, were left buckled after the earthquake, distorted by the intense ground motion. Earthquake Rubble. Date: 2nd march 1987 Magnitude: 6.5 Depth: 8 kilometers Death toll: … [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. Sign in Sign up for FREE Prices and download plans Lava Cracked Background. This survey helped gain an understanding of the shear wave propagation characteristics across an active fault in the sediments of the area. See earthquake stock video clips. 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. There is also the possibility of a third, significantly smaller, rupture another ten seconds later. 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. [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. The largest rupture, the Edgecumbe Fault, was 7 kilometres (4.3 mi) long and formed on, and extended, a late Holocene fault scarp. Minutes later a much stronger quake rocked the region. 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. Hdr Destroyed Area. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. The Pleistocene-to-Holocene Edgecumbe volcanic field covers about 260 km2 of Kruzov Island west of Sitka in the SE panhandle of Alaska. 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. ... sergeant of the marines on James Cook's Endeavour expedition. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. [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. The people standing nearby show the scale of the rupture. [8], The Rangitaiki Plains lie within the Taupo Volcanic Zone, which is widening. Prices and download plans . 205 Free images of Earthquake. 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 was the nearest centre to the magnitude 6.3 earthquake of 1987. Images courtesy of Frontier Helicopters. The main rift created by the earthquake. 130,711 earthquake stock photos, vectors, and illustrations are available royalty-free. These northeast trending tectonic ruptures are widely distributed across the Wellington Earthquake National Initial Response Plan version 1.1 now available Results of the Disaster Preparedness Survey for 2017 now available 157 172 16. [2][3] It appears that the fault has ruptured at least once previously in the past 1800 years. 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. [1][2], The main shock was preceded for two weeks by earthquake swarms in two areas of the Bay of Plenty. 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. Volcano Geography Views. Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … 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. Bay of Plenty Earthquake, 1987 (16552659081).jpg 3,734 × 2,511; 2.04 MB We’re continuing to work on improving the quality of our data, so please bear with us in the meantime. [3][5], Eleven ground-surface ruptures occurred in the Rangitaiki Plains, though no active faults had previously been recognised on the Plains. 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. Browse 1987 edgecumbe earthquake pictures, photos, images, GIFs, and videos on Photobucket The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. Site Quicklinks Culture & Society. 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