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Landslides in the Sydney Basin - Geoscience Australia

Landslides in the Sydney Basin - Geoscience Australia

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Seismic Hazard <strong>in</strong> <strong>Sydney</strong>Proceed<strong>in</strong>gs of <strong>the</strong> one day workshop<strong>in</strong> <strong>the</strong> <strong>Sydney</strong> area s<strong>in</strong>ce 1992 were under <strong>the</strong> Blue Mounta<strong>in</strong>s. Most events have been located to aprecision of a few kilometres or better, <strong>in</strong>clud<strong>in</strong>g depth. Although many near surface blasts and m<strong>in</strong>ecollapses have been recorded <strong>in</strong> coal m<strong>in</strong><strong>in</strong>g areas, very few earthquakes appear <strong>in</strong> <strong>the</strong> top fewkilometres. It is possibly that <strong>the</strong> Mesozoic sediments of <strong>the</strong> <strong>Sydney</strong> Bas<strong>in</strong> are too weak to susta<strong>in</strong>very high stress. The deepest earthquakes that have been precisely determ<strong>in</strong>ed are about 17 km deep.Figure 4: Vertical sections with earthquakes before 1992 (top) and 1992 to 1998 (bottom)Although <strong>the</strong> overall rate of earthquake activity for <strong>the</strong> region is not altered significantly by <strong>the</strong> newdata, a possible re-distribution is both reasonable <strong>in</strong> terms of geology and topography, and <strong>in</strong>dicatesthat <strong>the</strong> Blue Mounta<strong>in</strong>s region has a higher level of earthquake hazard than <strong>the</strong> <strong>Sydney</strong> region.Although <strong>the</strong> level of activity under <strong>the</strong> Blue Mounta<strong>in</strong>s is above average by <strong>Australia</strong>n standards, itis still far less than <strong>in</strong> <strong>the</strong> active earthquake areas of <strong>the</strong> world. The record<strong>in</strong>g period is very short53

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