  The seismicity of Greek region is studied under the prism of ESE & EDE
methods for finding the inflection point of cumulative energy released. Main
shocks are chosen from 106 years data. The result is that with both methods a
critical time region exist at the end of 1982 to early 1983. After this time
the seismicity tends to increase and gives remarkable events, like Athens Sep
1999 earthquake.
