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The earthquake of Skyros Island in Greece (26/7/2001, Ms = 6.1 R) wasannounced three days before its occurrence in a meeting organized by theBulgarian Academy of Sciences, Sofia on 2001. In this work a review is made onthe results of the methodologies which were used for the analysis of theavailable data in order to utilize the specific prognosis. Of particularinterest is the fact that the determined time of occurrence deviated for lessthan an hour (actually it was 41 minutes) from the actual occurrence time ofthe specific EQ. A similar example of another large EQ (Kythira, Greece, Ms =6.9R, 8th January, 2006) by using the very same methodology deviated for 43minutes only. The rest of the prognostic parameters: the epicenter location andthe magnitude of the Skyros EQ were utilized by manipulating the past seismicenergy release history of the regional seismogenic area and the observedearth's electric field which was recorded during the last 25 days, before theoccurrence of the large seismic event, by VOL earth's electric field monitoringsite. It is concluded that a short-term earthquake prediction can be utilizedas a really "short" one, once the available precursory data are processed withthe appropriate methodologies.

How "Short" a "Short-term earthquake prediction" can be? A review of the case of Skyros Island,Greece, EQ (26/7/2001, Ms = 6.1 R)