An earthquake of magnitude 4.4 at just 3 kilometers depth shook the Phlegraean Fields and Naples at 5:51 in the morning. The movement, one of the most intense since the resumption of bradyseism, recalled the magnitude 4.6 earthquake of June 30 of the previous year, the most violent in four decades. Social media filled with testimonies from residents awakened by creaking sounds and the rocking of their beds.
Seismic technology: sensors and early warnings 🌍
The INGV monitoring network recorded the event in real time thanks to a dense grid of accelerometers and seismometers deployed in the caldera. These devices detect P and S waves to calculate the epicenter and magnitude in seconds. Although the early warning system did not issue a public alert due to the low probability of structural damage, the collected data allows for refining ground deformation models and predicting possible short-term variations in bradyseismic activity.