The Flegraean Fields (also known as Campi Flegrei in Italian) are active volcanic fields near Naples, Italy. Unlike nearby Mount Vesuvius, Campi Flegrei does not have a single volcano. It is rather a volcanic system, with several centers located within sunken areas called calderas (essentially deep sinkholes or cauldrons).
Campi Flegrei is surrounded by suburbs and densely populated areas near the city of Pozzuoli. After a period of relative quiet and peace for the past 40 years, things began to change in September 2023.
Earthquakes began to be felt in Campi Flegrei in September 2023. Since then, more than 1,100 earthquakes have been recorded, some reaching 4.2 on the Richter scale. This caused the height of the ground to change. It is a process known as “Gradual earthquake“. The region has been affected by this phenomenon before, most recently from 1968 to 1972 and then again from 1982 to 1984.
Gradual earthquakes can cause the Earth’s surface to rise or fall when magma chambers buried 3 to 4 kilometers deep fill and empty in cycles of uplift and subsidence. This process causes the earthquakes felt by residents here.
However, the people who live here do not care about it, thinking that it is the “breath of the volcano” that lies beneath their eyes. Still, volcanologists have been studying calderas to predict what will happen in the future to avoid potential disasters.
Pisciarelli fumarole
fumaroles such as Pisciarelli fumarole, a vent on the earth’s surface that releases steam and hot volcanic gases such as sulfur dioxide and carbon dioxide. These can occur as holes, cracks, and fissures near active volcanoes or in areas where magma has risen into the Earth’s crust without erupting.
temple of serapis
The Temple of Serapis in Pozzuoli (which was a market building rather than a temple) is considered an emblematic monument of the Campi Flegrei region. It is a symbol of volcanic gradual earthquakes in this region. The ground beneath the surface is either rising or sinking, so it can be completely dry or half submerged in seawater.
The study of slow earthquakes over the past centuries has been made possible thanks to observations such as those made on the ruins of this Roman building. For example, by studying holes drilled into ancient columns by marine molluscs over centuries, scientists can study changes in sea levels at this site.
Source: www.sciencefocus.com
