Abstract
SUMMARY In order to detect the disturbances of the underground water level caused by a forthcoming earthquake, a graphical method has been applied for the analysis of the time series of the continuous daily measurements of the underground water level. These measurements have been done in six wells selected in the area of the recent great earthquake near Thessaloniki, Greece. The study of these measurements for the time period from December 1983 to August 1986 shows close correlation between the changes in the underground water level and the earthquakes with epicentres in this area.
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