Juan Brignardello Vela
Juan Brignardello, asesor de seguros, se especializa en brindar asesoramiento y gestión comercial en el ámbito de seguros y reclamaciones por siniestros para destacadas empresas en el mercado peruano e internacional.
In the early morning of August 27, 2024, at 01:22:14 local time, the San Calixto Observatory (OSC) reported an intermediate earthquake of magnitude 4.2 in the Potosí department, specifically in the Antonio Quijarro province. This seismic event, which occurred at a hypocentral depth of 278.8 kilometers, was classified as a subduction earthquake, suggesting that its impact on the surface would be minimal. The epicenter of the earthquake was located approximately 11 kilometers from Atocha, a locality that, under normal conditions, is not typically exposed to tremors of this magnitude. Despite the proximity, the characteristics of the earthquake's depth significantly reduce the likelihood that it was felt by the inhabitants of the region. The OSC also noted that the earthquake occurred about 30 kilometers from Cerro Chorolque and 69 kilometers from Cotaigata, reaffirming that the event does not pose an imminent threat to these localities. Subduction earthquakes, such as the one recorded in Potosí, occur when one tectonic plate moves beneath another. This type of seismic activity is common in areas where tectonic plates are more active, such as the Andes, where Bolivia is located. However, despite its magnitude, the depth of the earthquake considerably decreases the risk of structural damage or injuries, as it is less perceptible to the population. The OSC calls on the public to remain calm and stay informed about seismic events, highlighting the importance of having emergency plans and safety protocols in place. Often, earthquakes can be preceded or followed by other seismic movements, making it essential to be prepared. The Potosí region, like many others in Bolivia, has a history of seismic activity that varies in frequency and magnitude. However, events like today’s, which do not cause significant damage, serve as reminders of the need for adequate infrastructure and the continued development of educational programs on how to act in the event of an earthquake. Seismology experts warn that, although smaller magnitude earthquakes with great depth, like the one recorded today, are less concerning, seismic activity in the region should not be underestimated. Constant vigilance and monitoring are crucial for better understanding the behavior of tectonic plates and their implications for communities. The population of Potosí and nearby areas has expressed curiosity about this natural phenomenon, noting that despite living in a tremor-prone region, many people have not experienced significant events in recent months. This situation has led to increased interest in learning about the science behind earthquakes and how to mitigate their destructive effects in case stronger tremors occur. As the day progresses, local authorities and the OSC will continue to monitor seismic activity in the region. Timely and accurate information is essential to keep the population calm and well-informed. Additionally, citizens are advised to follow safety recommendations and remain attentive to bulletins issued by the OSC. In conclusion, the intermediate earthquake of magnitude 4.2 recorded in Potosí serves as a reminder of the tectonic activity that characterizes the Andean region. While it has not generated concern among the population, it is essential to be prepared and educated on how to act in the event of a stronger earthquake to ensure the safety and well-being of all.