For populating the subject 3D model, records of 100 earthquake events, that had occurred between 2007 to mid-2015 in an area of the Fleurieu Peninsula with the densest seismograph coverage, were selected from the South Australian earthquake catalogue. The event data were carefully checked, and some recalculations and deletions were applied to improve their quality. The earthquake magnitude layer displays event data ranging from the largest, a magnitude 3.8 occurring near Mount Barker in 2010, to the smallest, one of close to magnitude 0.0. These earthquakes have been located using a standard regional velocity model, not a local one. Changes caused by using a local model are expected to be relatively small, and affect all depths proportionately. The model includes the location of all the seismographs as at 2015. The surface elevation has been exaggerated 5 times to improve visibility. The displayed ‘area of interest’ polygon encloses the area with the densest seismograph coverage. Inside the polygon, hypocentres are generally more accurate. Poorer quality data have been removed. Hypocentres outside the polygon have not been included, because their accuracy decreases significantly. The ‘quake reliability’ layer shows the error ellipses (2 sigma) of the hypocentres, which demonstrate their possible location errors. The solid geology component of the model comes from the DSD spatial data library. The faults included are (from west to east): Para, Eden-Burnside, Ochre Cove, Willunga, Bremer and Palmer. Very little is known of the subsurface location of the major faults. The fault surfaces have been constructed using the mapped surface expression taken from the spatial data library, extrapolated at an angle of 45 degrees in the generally expected dip direction. The faults mapped at surface on the western side of the peninsula dip under the Mount Lofty Ranges. The Palmer Fault dips to the west. The Bremer Fault is expected to dip to the east. The fault positions are extended to 10 km depth in the model, except for the Bremer Fault, which has been extended to only 5 km depth. The subject visualisation model provides the first instance of an earthquake dataset for this particular area that is suitable to use for comparing the loci of earthquakes with geology and topography in 3D.