Every 25 minutes an earthquake in Korca

By the middle of yesterday, we have an almost drastic decline, d.m. We have very rare seismic activity on frequency, but also at the size of the magnitude, so in their strength. If we look at you until yesterday's evening, so the 3rd, we've had a micro-eventage every 25 minutes, which has had a magnitude of 2nd scale. Today, however, is characterized by almost no micrometers. In the early hours of the morning there were several microthers and these in the same size”, said Edmont Tushi, seismologist.

But the decline in activity, for seismologists, does not rule out an opportunity to reactivate the area.

“Nated by current data we have a decline, so activity is almost stopped, but this does not rule out the possibility of reactivating the area or activating another area because these are natural tectonic phenomena, which cannot be predicted”, said Edmont Tushi.

Sismologist says this is a classified area as seismogen area, and brings two previous earthquakes into focus with a high magnitude.

This area is classified by us as sysimiologist, a seismologen area, so capable of generating earthquakes. The last strong earthquake in the Korca area occurred in 1960, which affected all areas in question, so all areas around the city of Korca have suffered significant damage at that time he has had a magnitude 6 yet there have been later earthquakes, but not that size. Name here the earthquake in Barmas with an episcal between Erseca and Korca in 2004, which had a 5.4 magnitude, so comparable to the major impact of this series of earthquakes that occurred on June 1st of this year, and we had damage in that period, which was not as large as they are in this case, but that had destroyed homes, mainly in villages near the area of the field and impacts on the ground, cracks of roads or of the building walls of <111x>, said Tuschimologist Tuschim.

From the quake in the Korca area on June 1st, many dwellings were damaged, while the most affected village was that town of Floqi.