There is no end to the agony of the residents of Santorini, Amorgos and the other islands in the Cyclades who live in the rhythm of Enceladus for another day, as the seismic activity continued during the night of Wednesday to Thursday in the maritime area between Amorgos and Santorini .

According to data released by the Geodynamic Institute of the National Observatory of Athens, six more “weak” seismic vibrations (4.4, 4.3, 4.2, 4.4, 4.5 4.5 on the Richter scale were recorded ) The period between 04:00 and 05:30 (respectively, in reverse chronological order, at 05:23, at 04:48, at 04:45, at 04:27, at 04:24 and at 04:02) in the maritime area between Amorgos and Santorini.

In addition, seismographs recorded a “weak” seismic vibration of 4.3 on the Richter scale in the west-sinking of Anafi.

Earlier, three “weak” seismic vibrations, two size 4.1 and one 4 on the Richter scale, were recorded at 01:16, 00:59 and 00:57, according to the Geodynamic Institute.

Wednesday night at 9:09 pm, the most powerful vibration so far was recorded in the context of the ongoing unusual seismic seismic seismic in the maritime area south of Amorgos, with 5.2 on the Richter scale, always at the Geodynamic Institute. Seismologists pointed out earlier this week that so far, no earthquake has been recorded that the Lord could be described.

According to a study by the University of Athens, more than 6,400 earthquakes have occurred in the Santorini – Amorgos zone from January 26 to February 3. Of these earthquakes, 800 were over 2.5 degrees on the Richter scale.

At the same time, it is emphasized that the seismic activity so far in the Santorini-Amorgos zone is probably bearing the characteristics of an earthquake, as there is no earthquake clearly larger than all others, which could be described as the main earthquake.

At the same time, the island of Santorini and Amorgos have been deserted as there are few who have chosen to stay in their homes and businesses along with the few tourists.

Enceladus continues to hit the area with the seismic sequence remaining intense and stable.