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NEW RESEARCH REVEALS HIDDEN EARTHQUAKE TROUBLE SPOTS A team from the The 2005 Now the scientists from the Departments of Geology and Geography at the The scientists have pioneered use of the laser probe to map active fault systems in The Dr. Dickson Cunningham in the Department of Geology and Dr. Kevin Tansey in the Department of Geography collaborated on a NERC funded project to map the distribution of recently active earthquake-prone faults in the southeastern Alps in Their key research results are now published in the latest issue of Geophysical Research Letters. The work was further supported by a Masters student in Geography, Stephen Grebby. Dr. Cunningham said: "Locating earthquake-prone faults in forested mountainous regions and understanding the potential seismic hazard they pose to local population centers has always been a problem to geoscientists. "Many regions of the world have undiscovered seismically active faults hidden by dense forests, including Indonesia, India, NW North America, all Andean nations and the alpine countries of Europe. Unfortunately for people living in these regions, these faults can be ticking time bombs. "We have demonstrated that airborne LiDAR can be used in mountainous terrain to virtually deforest the landscape and reveal details of the forest floor topography, including the traces of active faults." Dr. Cunningham reports that the research involved collaborative efforts with Slovenian geoscientists and InfoTerra, a global geo-information supplier based in The topographic images derived from LiDAR data of two major plate boundary faults, the Idrija and Ravne strike-slip faults in He added: "For the first time, we are able to see how the faults connect at the surface and cut the landscape. This allows us to assess whether the faults are likely to produce large earthquakes or small events in the future. The images also allow efficient identification of sites suitable for detailed fault analysis to calculate the recurrence interval of major earthquakes and make probabilistic estimates of the timing and magnitude of the next major earthquake." A field excursion in August 2006 verified the remote observations. Dr. Tansey said: "As we trekked through the forest we found overwhelming evidence for previous fault activity, never before seen by earth scientists. We are now building on our initial results with follow-up research and have established the
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