Santorini earthquakes create panic in Greece, where local residents can erupt a volcano

The volcano erupted on the island of Santorini in 1866. Horseshoe shape was created for the island during a catastrophic eruption of 1500 BC. The old explosion may have created a wave of extension of the destruction of the city of Nosos Minoan on the island of Crete, and may also have led to the lost legend of Atlantis.

Printing mosque/Getty pictures

The Greek island of Santorini is located in the main headlines again, not because of the huge increase in tourism ships and cruises last season, but due to a squadron of severe earthquakes this week. With increasing concerns about a submarine Colombo volcano, 11,000 local population and visitors have recently left the island, and many wonder whether earthquakes could be launched from a possible eruption or form a new volcano.

The Greek government declared a state of emergency in Santorini this week, and it was required of the population and hotel owners to drain all swimming pools, because the water movement could shake build buildings. People were also directed to avoid old buildings. Small rock declines occurred along the slopes, prompting the Greek authorities to restrict access to the specific areas as high -risk. Discussions on evacuation plans began between the Greek authorities, as the population became increasingly afraid.

The Blue Dome Church along the edge of Caldira in Oi, Santorini

Gigantic

Scientists and researchers remain confident that the volcano will not pose a threat despite the report published in geological and geophysical chemistry and geological systems that reveal that the magma room that has not been discovered previously grows under the Colombo volcano that can lead to another eruption.

According to the report of the National Institute of Vevisers and Volcanology, “The affected area is one of the most active areas of the Hellenic Sagittarius. Current events occur along the Santorini-Famorgos rift area, known for its ability to generate high-sized earthquakes. The most destructive earthquake in the area in the area July 9, 1956, with a size of 7.1, followed by a strong tremor of 6.9, causing widespread damage and violent damage.

Modern geological studies have also highlighted a mistake with a recently exposed surface at the base of the sea bottom, compatible with the 1956 earthquake. “The combination of active tectonic and the presence of submarine errors involves a great danger of large -scale earthquakes, with possible effects on coastal societies and local infrastructure It represents the possibility of secondary phenomena, such as tsunami or the instability of the sea floor with the submarine landslides associated with the earthquake collapses caused by the earthquake on the surface, an additional weakness of the area. .

Clarify the details of the magma under the volcano in Santorini.

Noah Shamwell and Michelle Plato -Volcanicroots.org Kolumbo Volcano

Located on the northeastern side of Santorini, the Colombo volcano witnessed a large eruption in 1650. This eruption led to the formation of a new island, with lava flows extending towards the Santorini coast. In 1650, the eruption took out ash in distant places such as Turkey and produced perkluetic flows that led to the death of about 70 people in Santorini, along with a large number of livestock due to toxic gases. In addition, a tsunami is likely to happen during the collapse of the volcanic cone, causing damage to the nearby islands and dumping flat coastal areas, on the eastern side of Santorini, where ruins of the Roman era were discovered.

Historical explosions in Santorini formed new islands inside Caldira during the Mino eruption. In 2011-2012, Santorini went through a stage of disturbances, with increased seismic activity, earth abnormalities, and gas emissions changes from the Nea Kamena.

Residents and tourists are scrambling to leave the Greek island of phrases and aircraft after “a barrage” of tremors in Santorini, Greece on February 04, 2025.

Anadolu via Getty Images

Greek Prime Minister Mitsotakis addressed the nation this week after the strongest earthquake, and urged calm with confirmation that all the necessary precautions were taken to protect the population and visitors alike. The Greek Ministry of Tourism is now planning to respond to the treatment of the impact of tourism on the islands surrounding Santorini, including Amorgos, iOS, NAXOS and Anafi.

I spoke with Michelle Plato, an advanced research colleague in volcanic geophysics that provided more details about the risks of the earthquake and the risks of the volcano. “The current activity is on a set of defects that extend between Santorini and Amorgos. The biggest events in the sequence were 5.2. The main concern related to risks is the possibility of larger earthquakes. There is a lot of discussion in society about whether the larger earthquake will follow. It is the repetition of an earthquake of the year 1956, which is 7.8, which is the largest earthquake in Europe.

“At the present time, it seems unlikely that the activity will reach these high levels,” he added. “The ongoing events are not exactly the error that declined in 1956, but it is close to a near mistake and it seems more restricted in the geographical term. The possible scenario is that the maximum sizes will remain about 5.0, and the activity will be cleaned slowly over a few weeks. No one can predict what will happen We can only analyze possible scenarios and prepare for the best we can.

Greek Prime Minister Kiriacos Mitsotakis arrives in Santorini and receives information from individuals working in the region after Greece announced on Thursday an emergency in Santorini.

Anadolu via Getty Images

With regard to the danger of the other volcanic eruption, Paulatto adds, “There was some slight increase in activity in Kolumbo Volcano and Santorini Volcano, which is enough to ensure accurate inspection, but not enough to raise the level of volcanic alert. I don't know that in Kolumbo or Santorini. Some of the additional earthquake measuring devices were deployed.

If you start to become an increase in the epicenter, Plato says: “It is important to keep in mind that seismic crises in volcanoes do not always lead to an eruption. See, for example, what happened in 2011 on Santorini when there was a seismic squadron, The Earth is distorted, increased gas emissions on Nea Kamini, but no eruption followed.

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Santorini earthquakes

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