Santorini Greece earthquakes: Why did 8,000 cakes of the islands hit with similar Speed ​​Speed ​​errors and a dark history of 6.5

Scientists have discovered nearly 8,000 earthquakes in a little more than two weeks near Santorini Island with Greece. The unusual barrage of earthquakes that began in late January has raised the authorities' concern. They have announced the state of emergency in Santorini, one of the most popular tourist destinations in Greece

The largest of these tremors, which recorded 5.2, raised fears between both locals and tourists. In response, nearly 11,000 people were evacuated from the island by sea, with the help of phrases and airlines in this effort.

Santorini, a famous tourist destination known for its famous white and blue buildings, is part of the Cyclades of Islands group in the Aegean Sea. The islands have a dark and dangerous volcanic history that extends to 650,000 years. Although earthquakes are common in the area, the frequency and density of the recent earthquakes may cause widespread anxiety. The authorities also noticed the risk of larger tremors that could lead to tsunami. The memories of the Tsunami and 1956 re -restored the last earthquake to the great earthquake in 1956, causing a fatal tsunami. That disaster claimed the lives of 54 people and destroyed entire villages. Greek Prime Minister Kiriacos Mitsotakis urged citizens to remain calm, as the authorities have developed relief measures, including establishing tents in basketball courts and sending payment marks that advise people to remain formulating areas vulnerable to rock collapses. Experts ruled out the repetition of the 1956 earthquake. The researchers explained that the current earthquakes are the result of tectonic transformations instead of volcanic activity. Seismologists note that earthquakes occur in a small area, which is not commensurate with the model style of the main scheme sequence after the scheme. Earthquakes instead are associated with a hard -to -predict tectonic process and can decrease or escalate more. Tectonic transformations led to spider -like cracks and volcanoes, whether below or above the water. Techtoon activity in Aege. The earthquakes are the result of the tectonic movement in the Aegean Sea. The deep Hellenic trench to the south and west of Greece, causing an ancient piece of oceanic cortex in the scarf, is known for causing seismic activity. Constant stress from this movement separates Greece, which leads to the areas of rift and volcanic configurations in the region. Santorney himself has a long history of volcanic activity, including major explosions such as those in 1560 BC, which contributed to the collapse of the ancient civilization. Although the island's volcanic activity is still active, the current scientific assessments indicate that earthquakes are not related to volcanic explosions, but rather to tectonic forces in play.

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