Santorini earthquake risk assessing: What is Colom's stress and what role does he play?

Cououlb Lecisten has become a basic point of discussion in evaluating seismic risks about Santorini, especially after Greek seismic data. He cited him as a major factor in risk assessment in terms of Santorini earthquakes.

In his analysis of the continuous seismic activity in the region, Tselentis stressed the role of Coulomb in determining whether the main Amorgos error in the region is at risk of activation. While he pointed out that the current accounts indicate slight pressure on this error, he has warned that its activation is still a possibility.

Understanding coulomb

Coulomb Le Kingdom describes how stress re -tensions inside the Earth's crust after the movement of the earthquake or magma. Cououlb-Jots has been used for years in earthquakes to understand how earthquakes do each other.

It depends on the standard of counter failure, which states that the error will slip when the shear stress goes beyond (the force that drives the error to move) its resistance (friction and natural stress).

When an earthquake or volcanic activity occurs, stress is redistributed in the surrounding areas. In some cases, this increases the possibility of another earthquake by making a mistake closer to failure. In other cases, it reduces stress, and effectively delays seismic activity, according to the American geological survey.

How scientists use Coulomb's strain to assess the risk of earthquake

Seismologists use Cououlb Strain Models to predict how to affect any other earthquake in nearby rift systems. This approach was applied in many major seismic events.

In Santorini, according to Tselentis, the movement of the magma below the Kolumbo volcano exerts pressure on the upper geological and dandruff layers, which in turn leads to multiple smaller errors in the region. Tselentis estimates this accumulation of stress, under certain circumstances, can lead to an earthquake 6 size if it becomes a specific error in the area of ​​the earthquakes in a critical way. However, the seismologist notes that the main error in the area, Amorgos's mistake, has not yet been activated.

Restrictions and discussion about Coulomb models

While the Coulomb analysis is a tool that is widely used in seismology, it is still the subject of discussion. A study conducted in 2020 published in scientific reports (nature) used a case study to study whether to change Cououlb's strain that greatly affects Guetenberg-Richter, which describes the statistical relationship between the size of the earthquake and frequency. The study found that Coulomb does not significantly change this basic relationship, indicating that although it is useful, it may not be a final indication of earthquakes in the future.

Other main restrictions of Coulomb models include the following:

Complex rift reactions-re-distribution of stress are not uniform, and faults may respond to the unexpected uncertainty-often assumes Cououlb Stress models changes in immediate stress, but seismic events in the real world can reveal over the months, years, or even factors from dozens- Volcanic activity

Greek earthquake specialists, despite their difference in their evaluation and prediction of the situation in Santorini, all embraced the need for a comprehensive and based on data for continuous seismic swimming near Santorini and estimated that the situation can continue unabated for several months.

Tselentis and Santorini earthquakes

Tselentis recently resigned from the National Committee for the Evaluation of Seismic Risk, noting the political intervention in scientific work.

In his public data, he expressed his concerns about the continuous seismic activity about Santorini, focusing on the potential activation of errors in the region. His warning has sparked a debate about the Greek government's dealings with seismic risks and scientific independence of the country's earthquake's efforts.

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