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The seismicity, which took place at the Methoni seismogenic area, in the timeperiod of 20/2/2008 - 10/4/2008, is analyzed in terms of its location, time ofoccurrence and magnitude. Furthermore, it is compared to the tidal (T=14 days,T=1 day) lithospheric oscillation and to the epicentral area suggested by theanalysis of the Earth_s electric field registered on 21-22/2/2008 by PYR, ATHand HIO monitoring sites. Moreover, a comparison is made between the actualseismic energy released, during the same time period (20/2/2008 - 10/4/2008) inthis specific seismogenic region and the suggested one by the probabilisticsingle seismic event suggested that could occur in the time period of 28/2_1/3/2008.  The overall analysis of the Methoni seismic event reveals the validity of theused physical models: of the lithospheric oscillation, of the lithosphericseismic energy release and the one of the homogeneous Earth used for theazimuthal intensity vector analysis of the preseismic electric signals(Thanassoulas, 2007).

Seismicity observed, at Methoni seismogenic area, Greece, after the  analysis of the recorded Earth_s electric field of 21/2/2008_ 22/2/2008, at  PYR, ATH and HIO monitoring sites, Greece