2012 gippsland earthquake cause

[5][6] It was felt across much of Victoria and parts of New South Wales, with strong shaking reported across the state capital, Melbourne. / Natural Hazards and Risks The 55-year-old said small earthquakes were “fairly common” in the area and he had easily experienced more than a dozen since moving to Korumburra 20 years ago. “In the centre, people have reported a low rumbling following by the rattling of objects. This raised part of the Port Hills and part of southern Christchurch. / Recent Events Over the next few seconds the rupture spread upwards and towards the northwest, with the amount of slip increasing with time. 2012 Gippsland earthquake is within the scope of WikiProject Australia, which aims to improve Wikipedia's coverage of Australia and Australia-related topics.If you would like to participate, visit the project page. However, there may be additional subsidence as a result of ground compaction and liquefaction during the strong shaking. [9], A magnitude 4.3 Mw aftershock occurred in the same area at 7.11 pm on 20 July 2012 at a similar depth. Colours on the fault plane indicate the amount of slip between the two sides of the fault (see Fig. 1). Home

A magnitude 4.9 earthquake struck Gippsland near Moe at 8.55 pm on 19 June 2012, at a shallow depth of 10.0 km. The nearby Latrobe Valley town of Moe was hit by a 3.2-magnitude earthquake in October and in June 2012 experienced a damaging 5.4-magnitude event. The images can be combined to show the total amount of shift of the ground surface, both vertically and horizontally, caused by the earthquake (see Fig.

I ended up with two scared dogs in bed with me.”. Central, northern and northeastern Christchurch have also gone down, but generally by less than 5 centimetres. It will enhance any encyclopedic page you visit with the magic of the WIKI 2 technology. / Our Science This is also known as Online Behavioural Advertising. A number of techniques were used to determine the fault’s position and movement. Alex Rosen, University Clinic Düsseldorf, Department of General Pediatrics Abstract The Tōhoku earthquake on March 11 th, 2011 led to multiple nuclear meltdowns in the reactors of the Fukushima Daiichi nuclear power plant in Northern Japan. We expect that details of the fault location and slip distribution will be updated in the future, as we incorporate more data and use more sophisticated data analysis techniques. The fault is not a vertical cut through the earth, but rather it dips towards the south at an angle of about 65 degrees from the horizontal. Don't have an account? Low This article has been rated as Low-importance on the project's importance scale. However, the violent magnitude 6.3 earthquake that devastated Christchurch on 22 February 2011 was caused by movement along a fault that does not appear to have broken the surface. It did not appear his home had suffered any damage. It will enhance any encyclopedic page you visit with the magic of the WIKI 2 technology. “People have mentioned that there was activity for about 10 seconds.”. Each colour cycle represents 1.5 centimetres of ground displacement, so the total displacement between the western edge of the image and central Christchurch is about 25 centimetres. Figure 2: Diagram showing the amount and direction of slip of the rock between the two sides of the fault. Movement was modelled using the ground shaking recorded during the earthquake by “strong-motion” seismometers. It was the strongest recorded in Victoria in at least three decades, with some sources suggesting it was the strongest in over a century. Position data from GPS stations (Fig. Figure 1: This Google map image shows the fault plane (rectangular area) across the southern part of Christchurch and northern Port Hills.

This type of fault motion is called reverse faulting. GeoScience spokesman Chris Thompson said the earthquake was not strong enough to cause any damage or injuries, but caused “quite a decent shake” — enough to rouse people from their sleep. [8] Approximately 60 aftershocks were recorded the following day, but most of these were not felt. Quite the same Wikipedia. The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple.

Because the fault doesn’t break the surface, the land overlying the top of the fault has been slightly folded, with the south side warped upward and the north side down (see Fig. The red star shows the location where the fault rupture started.

The coloured image shows an “interference pattern” derived from X-band radar images taken on 19 and 23 February 2011 by the Italian Cosmo-SkyMed satellite. 1) was about 14 kilometres long, and extends east-northeast from Cashmere to the Avon-Heathcote estuary area.

AN earthquake that struck a South Gippsland town overnight, shaking items of tables and rousing sleeping residents, was reportedly felt as far away as inner-Melbourne. Boyd Maddocks, who lives just metres from the epicentre, told the Herald Sun the quake had jolted him from his sleep and caused his whole house to shake. The 3.4-magnitude quake hit just after 3.30am in Korumburra, a town 120km southeast of Melbourne, according to GeoScience Australia. These instruments are designed specifically for recording strong ground shaking. This article describes our understanding of the Christchurch earthquake fault as at the 8th of April, about 7 weeks after the earthquake. “Objects have moved, fallen off tables,” she said.

March 9 th, 2012 Dr. med. Just better. “If people are in tall buildings, they’re likely to experience shaking that’s a little stronger. The greatest movement was upward and toward the northwest under the Avon-Heathcote estuary area. “My iPad fell off the charger. “So people in apartments in Flemington may have felt it.”. 1) was about 14 kilometres long, and extends east-northeast from Cashmere to the Avon-Heathcote estuary area. You can find out more about our policy and your choices, including how to opt-out

AcknowledgementsFor discussions and sharing of early results: Pierre Briole, ENS, France; Marcello de Michele, BRGM, France; Eric Fielding, JPL, USA; SARmap group, Switzerland; INGV, Italy; GSI, Japan; Shaun Levick, Caroline Holden, Bill Fry, Stephen Bannister, Martin Reyners, all at GNS. The white line is the contour where there was no change in height. Free kinder announced; 11th ‘double doughnut’ day in a row, Aussie shares climb to new high on COVID-19 vaccine hope, Cops could be jailed over misconduct in Silk-Miller case, PM slams ABC’s ‘absurd’ probe into affair allegations. An earthquake is caused by a sudden slip on a fault.The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. You could also do it yourself at any point in time. here. Based on data from GPS stations, satellite radar images, seismographs and strong-motion recorders, the fault that caused the 22 February earthquake lies within about six kilometres of the city centre, along the southern edge of the city. 2).

This earthquake produced a visible rent across the landscape that allowed scientists to directly measure the movement of the longest fault segment, the Greendale Fault. South-east Victoria has been rocked by more than 40 aftershocks after a magnitude-5.4 earthquake hit near Moe in Gippsland on Tuesday night.

[10] This aftershock is the strongest so far of over 200 that have occurred since the initial quake.[11]. Fellow GeoScience seismologist Emma Mathews said the agency had received reports of shaking from residents as far away as Flemington — about 120km from the epicentre in Korumburra’s southwest — and Blackburn — more than 100km away. Fault slip comes to within one kilometre of the ground surface.

2012 Gippsland earthquake. The main part of the fault thus lies beneath the northern edge of the Port Hills. “It was like the sound of a really big truck coming past — first you get that distant rumble, then you feel a bit of a shudder. / Hidden fault. The fault rupture (Fig.

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“We’ve had reports from the local area of Korumburra, Drouin, Leongatha, Warragul, and further west in Pakenham, Blackburn, Dandenong, Monbulk and Flemington,” Ms Mathews said. It felt like an explosion under your feet,” he said. The red, green and yellow coloured symbols show some of the GPS stations whose displacements were used to derive the fault slip model. That's it. Congratulations on this excellent venture… what a great idea! Two aftershocks — one 10 minutes after the initial quake and another an hour later — had also been reported to GeoScience. It was felt across much of Victoria and parts of New South Wales, with strong shaking reported across the state capital, Melbourne. GeoScience had received about 60 “fault reports” from people who had felt the quake by 7am. The suburbs of Heathcote and Redcliffs lie above the fault, resulting in heavy damage and extensive rockfalls.

The contour lines indicate the amount (in mm) the land has risen (blue contours) or subsided (red contours) due to the slip on the fault. He said his house shook for at least four seconds, but it felt like much longer.

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