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The Earth's preseismic oscillating (T = 24h) electric field recorded for ashort-time period of some days is analyzed in terms of its intensity vectorazimuthal direction calculated at one monitoring site. The calculated azimuthaldirections are compared to the concurrent seismicity observed for the sameperiod of time. Examples are presented for proving the agreement between theelectric field intensity vectors calculated azimuths and the corresponding onesreferring to the EQs - monitoring site location. Finally, an example ispresented on account of the use of this methodology upon three differentmonitoring sites for the utilization of the estimation of the epicentral areaof a large future EQ at the Methoni, Greece seismogenic area.

Multidirectional analysis of the oscillating (T = 24 hours) Earth's electric field recorded on ground surface