An earthquake measuring 4.6 on the Richter scale shook the Greek town of Elassona, located near the city of Larissa in Thessaly, on Tuesday evening.
According to the Greek Geodynamic Institute, the epicenter of the earthquake was located 14 km (8.7 mi) south west of Elassona.
A few small seismic events had been recorded in the region on Tuesday afternoon, the Geodynamic Institute noted. No damage or injuries have been reported.
In March, the region was hit by a strong earthquake measuring 6.0 on the Richter scale. Several buildings in the town were completely destroyed after the quake, and many residents had to flee their homes.
The worst hit village in the area was Mesohori, near Elassona where the local church and some old houses were badly damaged in March.
Greece is earthquake prone
Greece lies in a highly seismically active region. The vast majority of earthquakes cause no damage or injuries.
The country is located in a complex boundary zone in the eastern Mediterranean between the African Plate and the Eurasian Plate.
The northern part of Greece lies on the Eurasian Plate while the southern part lies on the Aegean Sea Plate.
The Aegean Sea Plate is moving southwestward with respect to the Eurasian Plate at about 30 mm per year while the African Plate is subducting northward, beneath the Aegean Sea Plate, at a rate of about 40 mm per year.
The northern plate boundary is a relatively diffuse divergent boundary while the southern convergent boundary forms the Hellenic arc.
These two plate boundaries give rise to two contrasting tectonic styles, extension on east–west trending fault zones with strike-slip tectonics on SW-NE trending fault zones throughout west and central Greece, Peloponnese and the northern Aegean and contractional in the southern Aegean, continuing around to the Ionian islands.
The south Aegean is the location of the volcanic arc and is characterized by extension. To the east of Crete along the Hellenic Arc, strike-slip tectonics with some extension become important.