Researchers from The University of Melbourne are learning how to modify existing Indonesian and Australian ports so earthquakes don’t do such devastating damage to sea trade.
“What we currently have is a recipe for disaster. Some of the port infrastructure is over 100 years old and wasn’t designed to cope with the loads they are currently bearing, let alone an earthquake,” says Dr Massoud Sofi.
The work of Indonesian and Australian scientists is resulting in re evaluation of Jakarta’s seismic risk by Indonesian Government agencies.
The team is scanning the Earth from thousands of kilometres in the air, right down to chemical traces found in rocks, as they hunt out telltale signs of future earthquakes and the damage they might do. They’ve highlighted a major new seismic threat for East Java as well as the tsunami threat to Bali, Lombok, Nusa Tenggara, and other coasts along the Flores Sea; and have identified active faults in the Nusa Tenggara region of Eastern Indonesia, measuring the rates of strain building up.
Ninety-nine per cent of all tsunami-related deaths have occurred in the Asia-Pacific region, according to the United Nations Economic and Social Commission for Asia and the Pacific. Indonesian and Australian scientists have been working to reduce this figure—by creating artificial earthquakes and tsunamis.
Building off more than 15 years of research from Indonesian, Singaporean, American, and Australian scientists, the team created a collection of scenarios, for earthquakes of different magnitudes and the resulting tsunamis that would affect West Sumatra, Indonesia.
Japanese researchers are coming to Australia for our neutron beams. It’s helping them continue their research following the shutdown of all Japanese research reactors in the aftermath of the Great East Japan Earthquake. And it cements a friendship in beamline science that kickstarted Australian access to synchrotron light.
“Japan’s leadership in electronics, advanced manufacturing and computing complements Australia’s leadership in agriculture, health and minerals,” says the Australian Nuclear Science and Technology Organisation’s (ANSTO) Robert Robinson, who chaired an Australia Japan Neutron Science Workshop in 2013.
The collaboration is contributing to research into: hard magnets for electric cars; new high density plastics; superconducting cables for the ITER fusion reactor; and the structure of a range of biological molecules.
Working together, researchers in Japan and Australia are getting better at predicting the areas most at risk from earthquakes.
They are also working together on ways to determine, within seconds of a warning, the scale and likely impact of an earthquake.
Rapid detection and warning systems combined with smart engineering saved many lives in the Great Japanese Earthquake of 2011. But the earthquake and the resulting tsunami were much bigger than geological modelling suggested. The reasons for that might be found in deep history.
Mapping the hazard
Big earthquakes may be separated by centuries or millennia. But earthquake hazard maps are based on information gathered since 1900 when modern seismographs came into use. It’s difficult to model events happening over millennia when you have not got deep historical information. Continue reading Reducing the impact of earthquakes→
Japanese researchers are coming to Australia for our neutron beams. It’s helping them to continue their research following the shutdown of all Japanese research reactors in the aftermath of the Great East Japan Earthquake. And it cements a friendship in beamline science that kickstarted Australian access to synchrotron light.
We know more about the topography of Mars than that of Earth because 70 per cent of our planet is covered by water.
Now University of Sydney PhD student Kara Matthews has used satellite data and GPlates, a computer package developed at the University, to create a complete digital map of the many geological features of the seafloor.
Fracture zones—the orange lines in the accompanying image—are deep linear scars on the seafloor that extend perpendicular to the boundaries where tectonic plates are moving apart, revealing up to 150 million years of plate movement. They are accompanied by huge ridges on the seafloor, rising up to 2 km above the abyssal plains, and valleys as deep as 8 km below sea level. Continue reading Mapping the seafloor from space→
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