A 5.2 magnitude earthquake struck lower than eight miles south-southwest of Néa Poteídaia, Greece, close to the island of Halkidiki on Sunday night. With a depth of 6 miles, its shaking could possibly be felt so far as Northern Greece, Bulgaria, Türkiye, and North Macedonia, in line with USGS.
The quake struck at 7:03 p.m. (native time) on Sunday night; its epicenter was roughly 7.5 miles southeast of the village, Nea Moudania. Shortly thereafter, at 7:07 p.m. (native time), a powerful aftershock was recorded at 4.3 magnitude on the Richter scale, and a 3rd at 2.8 magnitude 5 minutes later.
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No Damages to Properties or Accidents. Nonetheless, Residents Are Fearful {That a} Bigger Quake Might Hit
Halkidiki, Greece
Fortunately, as robust and as shallow because the preliminary earthquake was, there have been no experiences of injury or accidents, per police and hearth service officers. Undoubtedly, the residents within the space are strolling round in a state of concern after three back-to-back quakes.
Professor of Geophysics at Thessaloniki College, Seismologist Kostas Papazachos acknowledged: “The concern will not be justified. Such earthquakes are quite common within the area; 15-20 happen yearly. It shouldn’t concern us as a result of it’s an space of comparatively low seismicity, and we should not have massive faults. The aftershock sequence is wealthy, and within the coming weeks, residents will really feel earthquakes and will put together. It isn’t unlikely {that a} robust aftershock of 4.6, or 4.8 might happen.”
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Because the African and European Tectonic Plates Proceed to Collide, Extra Earthquakes Will Happen within the Future
Messina Strait separating Messina, Sicily and Reggio di Calabria
Greece lies between two unstable, converging tectonic plates: the African and the European. Their proximity to at least one one other, and steady collisions trigger earthquakes fairly regularly in Greece and the encompassing international locations.
In line with experiences by National Geographic, ‘research of current earthquakes within the area point out {that a} new subduction zone could also be forming the place the plates are colliding alongside the coasts of Algeria and northern Sicily.’
The final main earthquake to hit Sicily was on December 8, 1908, when a 7.1 magnitude struck throughout the Messina Strait, the slim water channel that separates Sicily and Calabria. 70,000 individuals had been killed as a result of quake’s drive producing a tsunami with waves 40 ft in top.
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