Seismic Hazard <strong>in</strong> <strong>Sydney</strong>Proceed<strong>in</strong>gs of <strong>the</strong> one day workshopoccur to <strong>the</strong> north and south and which mark <strong>the</strong> edges of <strong>the</strong> two plateaux, <strong>the</strong> Hornsby andWoronora Plateaux. To my knowledge <strong>the</strong>se structures, which by my suggestion of formation arema<strong>in</strong>ly contemporaneous with <strong>the</strong> major formation of <strong>the</strong> Lapstone structures, show no evidence ofreverse movement on any large scale. The curvature of <strong>the</strong>se structures as <strong>the</strong>y sw<strong>in</strong>g easterly seemsto conform with a fairly simple pattern of downdragg<strong>in</strong>g of <strong>the</strong> central bas<strong>in</strong> (Figure 3).Although it might be simplistic, one would expect a strong thrust<strong>in</strong>g from <strong>the</strong> west to producesympa<strong>the</strong>tic curv<strong>in</strong>g of faults westerly at <strong>the</strong> north and sou<strong>the</strong>rn extensions of a strong north-southtrend<strong>in</strong>g thrust, ra<strong>the</strong>r than what we now map.CONCLUSIONSThere is much still to learn about <strong>the</strong> structural nature and tectonic history of <strong>the</strong> <strong>in</strong>ner (andtotal) <strong>Sydney</strong> Bas<strong>in</strong>. It is pleas<strong>in</strong>g that this task is be<strong>in</strong>g taken up with vigour by geologists andgeophysicists. It will surely bear fruit and contribute to <strong>the</strong> rais<strong>in</strong>g of safety standards with<strong>in</strong>and extend<strong>in</strong>g beyond <strong>the</strong> metropolis, particularly with respect to seismicity.REFERENCESAndrews, E.C., 1910. The Tertiary unity of eastern <strong>Australia</strong>. Journal and Proceed<strong>in</strong>gs of <strong>the</strong> RoyalSociety of New South Wales, 44, 420 - 480.Bembrick, C.S., Herbert, C., Scheibner, E. and Stuntz, J., 1973. Structural sub-division of <strong>the</strong> NewSouth Wales portion of <strong>the</strong> <strong>Sydney</strong> – Bowen Bas<strong>in</strong>. New South Wales Geological SurveyQuarterly Notes 11, 1 – 13.Branagan, D.F., 1975. Fur<strong>the</strong>r thoughts on <strong>the</strong> Lapstone Structure. 10th Symposium on Advances <strong>in</strong><strong>the</strong> Study of <strong>the</strong> <strong>Sydney</strong> Bas<strong>in</strong>, Abstracts. Department of Geology, University of Newcastle,22 – 23.Branagan, D.F., 1977. Faults <strong>in</strong> <strong>the</strong> Hawkesbury Sandstone, 1977 11th Symposium on Advances <strong>in</strong><strong>the</strong> Study of <strong>the</strong> <strong>Sydney</strong> Bas<strong>in</strong>, Abstracts. Department of Geology, University of Newcastle,20.Branagan, D.F., 1985. An overview of <strong>the</strong> geology of <strong>the</strong> <strong>Sydney</strong> Region. In Pells, P.J.N., (ed.)Eng<strong>in</strong>eer<strong>in</strong>g Geology of <strong>the</strong> <strong>Sydney</strong> Region. Rotterdam: Balkema, 3 – 48.Branagan, D.F., 1991, Pyrmont Geology. 25th Symposium on Advances <strong>in</strong> <strong>the</strong> Study of <strong>the</strong> <strong>Sydney</strong>Bas<strong>in</strong>. Department of Geology, University of Newcastle, 162 – 169.Branagan, D.F., 2000a. The Hawkesbury Sandstone: its orig<strong>in</strong>s and later life.In G.H. McNally andB.J. 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