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The recent large EQ that occurred in Greece (April 1st, 2011, Ms = 6.7R) isinvestigated as far as it concerns regional geophysical features of the Greekterritory. In particular, the EQ location is compared to the deep lithosphericfracture zones and faults, derived from the analysis of the correspondingearth's gravity field; to the current seismic potential map determined from thestudy of the past seismicity, while its time of occurrence is compared to thepeaks of the M1 and diurnal tidal waves. The detailed investigation of theearth's electric field that was recorded by the ATH monitoring site, located inAthens, revealed the presence of short train like pulses type electric seismicprecursory signals which were generated short (1 - 2 days) before the EQoccurrence time. Moreover, the analysis (for T = 1 day) of the earth'soscillating electric field, that was simultaneously recorded at PYR and ATHmonitoring sites, revealed that the "strange attractor like" seismic electricprecursor preceded for 1 - 2 days the EQ occurrence time. A similar behaviorwas observed from the large EQ of the East Kythira (Ms = 6.9R, January, 8th,2006). It is concluded that the same regional tectonic mechanism controlled andgenerated both the analyzed EQs while the adopted geophysical earth models havebeen validated.

On the recent large EQ of Karpathos, Greece (April 1st, 2011, Ms = 6.7R)  and its similarities to the large EQ of the January 1st, 2006 (Ms = 6.9R) at  East of Kythira, Greece