One of the most characteristic areas is the seismic park, a phenomenon that took place 3500 years ago after an earthquake with a magnitude of 6.8 on the Richter scale. The movement brought a part of the sand and water up, giving them a cylindrical shape, known as seismites.
The “seismites” are geological formations with a strange morphology that occur in this area of El Médano. They are a type of tubular sandstone structures that rise from the ground, and although they go unnoticed if you are not paying attention, they become quite striking once you notice their existence.
The Seismic Park of Montaña Roja, located in the nature reserve surrounding Montaña Roja, is an important research and education area focusing on seismic activity and volcanic phenomena.
The park is equipped with advanced seismic instruments that continuously measure the seismic activity in the region. This helps scientists monitor and study earthquakes and volcanic activity. Geologists and seismologists collect data on seismic waves, earthquakes, and other geophysical phenomena to better understand the dynamics of the Earth's crust in the area. Through ongoing monitoring and analysis of seismic activity, the park contributes to the safety of the region. It can provide early warnings for possible volcanic eruptions or earthquakes, allowing preventive measures to be taken to protect the population.
The park has a educational function, where visitors can learn about seismology, volcanology, and the geological history of Tenerife. There are information boards and educational materials available to raise public awareness about the dangers and the science behind earthquakes and volcanic eruptions.
Source: Willem Vandenameele - ChatGPT
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