Earthquake in the Tyrrhian Sea: Secrets of the Earth Pan Movement!
Earthquake in the Tyrrhian Sea: Secrets of the Earth Pan Movement!
Tyrrhenisches Meer, Italien - On April 28, 2025 at 9:39 p.m., an earthquake in the southern Tyrrhenian Sea occurred with a magnitude of 3.6. The epicenter was at sea between the coast of Calabria and the Aeolian Islands, at a depth of 169 kilometers. Due to the large depth and the location on the open sea, there were no damage, although the quake in the provinces Reggio Calabria and Messina was noticeable, especially on the upper floors of buildings. This region is geologically active and is characterized by numerous volcanoes such as the Etna and the Stromboli as well as frequent earthquake events. In recent years, two comparably stronger earthquakes have been recorded here, with a magnitude of 7.1 being registered with a magnitude of 7.1 in 1938.
The accumulation of these seismic activities is also due to the geological conditions. One speaks of the defined Wadati-Benioff zone, an inclined plane where the ionic plate is pushed under the continental plate of Europe. This movement is part of the complex event of platter tectonics, which explains the movements of the continental plates and the associated earthquakes and volcanic eruptions. The African plate continues to move towards the Eurasian plate, which could lead in the long term to close the Mediterranean.
geological background
in the Wadati-Benioff zone, which was named after the seismologists Hugo Benioff and Kiyoo Wadati, most earthquakes take place in subduction zones. This zone can have seismic activities in depths of up to 670 kilometers. The earthquakes are mostly the result of glide along the subduction over shifts or within the diving plate. It is noteworthy that the earthquakes up to 300 kilometers deep are primarily generated by dehydration reactions within the panels.
The depth in which these earthquakes occur also offers valuable information about the structure of the diving oceanic crust and the upper coat. The earthquake in the Tyrrhian Sea is another sign of the complex geological processes based on this region. Historically, Africa has been moving towards Europe for 100 million years, which ultimately led to the emergence of the Mediterranean.
conclusion and other earthquake activities
It is worth noting that there have been further earthquakes in the region in recent months, including events in May and February 2025, which also took place at great depth. The movements that manifest themselves with these earthquakes are often associated with the geological processes in the Wadati-Benioff zone that are not to be underestimated under the region's historical forces. In view of this geological dynamic, the region around the Tyrrhenian Sea is a special area of interest for scientists. The research of seismic activities in connection with the plate tectonics could be crucial for the long -term understanding of the earth's crust in this active geological zone.For further information on the geological conditions and the underlying mechanisms of the Wadati-Benioff zone, we refer to the extensive explanations in the articles of Merkur href = "https://en.wikipedia.org/wiki/wadati%80%93benioff_zone"> wikipedia (English) and wikipedia Information) .
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| Ort | Tyrrhenisches Meer, Italien |
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