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Published online by Cambridge University Press: 03 November 2011
In a recent issue of this journal, Crampin (1998) suggested that analysing seismic shear-wave splitting along appropriate ray paths can be used to monitor the build-up of stress before earthquakes. If the source and recording geometry are suitable, this procedure, known as stress-forecasting, allows the approximate time and magnitude, but not the location, of future large earthquakes to be estimated.