edgecumbe earthquake images

Liquefaction of Cohesionless Soils in the March 2, 1987 Edgecumbe Earthquake, Bay of Plenty, New Zealand, and other Earthquakes. [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. [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. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. 109 82 19. Although not of an exceptional magnitude, it was damaging because it was very shallow. Share this item Post to Pinterest Post to Facebook Post to Twitter. Find the best free stock images about earthquake. ... Damage to the wall foundations during the 1987 earthquake may have also been a contributing factor. Edgecumbe Earthquake, N.Z., 1987 Edgecumbe Earthquake, N.Z., 1987; Filter By Type All Results 31. 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." The people standing nearby show the scale of the rupture. A DigitalNZ story by: David Clover - Images of the Edgecumbe earthquake 1987 It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. 400 445 52. [8], The Rangitaiki Plains lie within the Taupo Volcanic Zone, which is widening. The Edgecumbe Fault. 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… Minutes later a much stronger quake rocked the region. The M6.5 event was soon named after the town. 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 Pleistocene-to-Holocene Edgecumbe volcanic field covers about 260 km2 of Kruzov Island west of Sitka in the SE panhandle of Alaska. Download all photos and use them even for commercial projects. [1] The hypocentre was at a shallow depth of 8 km. 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. Buckled railway line and a locomotive flung on its side by the force of the Edgecumbe earthquake. Kaikoura Earthquake and Tsunami: 14 November 2016 Post Event Report (National Emergency Management Agency response) Exercise Tangaroa post-exercise report. [2][3] It appears that the fault has ruptured at least once previously in the past 1800 years. An earthquake measuring 6.2 on the Richter scale struck Edgecumbe on 2nd March 1987. Brick Brickwork Ruin. 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. 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. Minutes later a much stronger quake rocked the region. The largest rupture, the Edgecumbe Fault, was 7 kilometres (4.3 mi) long and formed on, and extended, a late Holocene fault scarp. ... All images & media in this story. 70 81 15. 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 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 … Multiple massive earthquake hit Japan on 11th of March 2011. 68 98 8. Toppled by the shaking. Steven A Christensen, Dept of Civil Engineering, University of Canterbury (EQC funded report 93/136) Abstract. Mt. Prices and download plans . The hypocentre was at a shallow depth of 8 km. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. The earthquake had been caused by movement along the fault; the land to the north-west had dropped by up to 2 metres. Media in category "Edgecumbe earthquake (1987) at Archives New Zealand" The following 10 files are in this category, out of 10 total. Date: 2nd march 1987 Magnitude: 6.5 Depth: 8 kilometers Death toll: … 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. 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], Twenty-five people suffered injuries that needed medical attention, but no-one was killed. 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. earthquake images. During the Edgecumbe earthquake, the area widened by 1.2 metres. 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 first was off the coast of Miyagi, the second was of the In the Edgecumbe rail yards an 80-tonne locomotive lies on its side. 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. ... sergeant of the marines on James Cook's Endeavour expedition. 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. 55 54 10. The slip on the fault induces a difference in the phase registered by the satellite Orbit 1 Orbit 2 (after an earthquake) Phase Four aftershocks with magnitudes greater than 5 occurred in the next six hours, and smaller aftershocks were felt for weeks. This survey helped gain an understanding of the shear wave propagation characteristics across an active fault in the sediments of the area. These northeast trending tectonic ruptures are widely distributed across the Four aftershocks with magnitudes greater than 5 occurred in the next six hours, … If something is not clear or seems incorrect, don’t hesitate to contact us using the online enquiries form. [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. Previous To … 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. [6] The largest aftershock measured 5.6 and struck nine minutes later at 1.51 pm. Wellington Earthquake National Initial Response Plan version 1.1 now available Results of the Disaster Preparedness Survey for 2017 now available Earthquake Rubble. See earthquake stock video clips. This Television New Zealand news coverage of 2 March 1987 reports the aftermath of the Edgecumbe earthquake. As these images are from the Ministry of Civil Defence, Central Regional Office. 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). 4 Jan 21:07 UTC: First to report: GEONET (NZ) after 2 minutes. 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. 205 Free images of Earthquake. The devastated Bay of Plenty town of Edgecumbe as photographed from the air. [3][5] The main shock appears to have actually consisted of two ruptures, and possibly a third. 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. 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. Earthquake in Japan 11th March 2011. Edgecumbe was the nearest centre to the magnitude 6.3 earthquake of 1987. Edgecumbe is a small town of around 1800 people, 18km west of Whakatane. [1][2], The main shock was preceded for two weeks by earthquake swarms in two areas of the Bay of Plenty. The most spectacular effect of the Edgecumbe earthquake was the 7-kilometre-long rift that appeared across the Rangitāiki Plains – the Edgecumbe Fault. There is also the possibility of a third, significantly smaller, rupture another ten seconds later. 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