A massive tsunami in Chile forced people away from the coast for 1,000 years!

3,800 years ago, a 9.5-magnitude earthquake had triggered a massive tsunami destructive to the coast of Chile. Prehistoric people had taken refuge inland, preserving the memory of this catastrophe for nearly 1,000 years.

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[EN VIDÉO] Kizaku: The Secrets of Creating Tsunamis
Tsunamis are among the most devastating natural disasters. These waves, which could be up to thirty meters high, hit the coasts with an unstoppable force. Unisciel and the University of Lille 1, through the Kézako program, reveal to us the secrets of the creation of this phenomenon.

The western coast of South America, due to its position in convergent plate boundaries, is at high seismic risk. Each year, the subduction of the Nazca oceanic plate under the South American continental plate is already responsible for many earthquakes, some of which can be very strong. The most powerful earthquake in modern history It was recorded off the coast of Chile in 1960. With the estimated amount of Mw 9.5This is amazing Earthquake led to an increase in floor A circumference of six meters in some places, causing violence tsunami. Waves 10 to 12 meters high swept the Chilean coast, sweeping away everything in its path and killing 3,000-6,000 people.

A tsunami is sure to be very deadly for the prehistoric people who live on the coast

However, this tectonic context is not recent and has presented significantly Birth in the Andes Mountains. It is possible that such seismic events, of somewhat similar amplitude, have already occurred in the past. A team of researchers also provides evidence that a huge tsunami struck the Chilean coast about 3,800 years ago. The results of the study were published in science progress, indicates that the strength of the earthquake at the origin of this tsunami should be comparable to that of 1960. However, at that time, Chile was already occupied by groups of fishermen – gatherers – fishermen who lived along the coast. Extremely vulnerable situation in the event of a tsunami. Scientists also showed that after this catastrophic event, the population had deserted the coast to settle within ground. This situation could have lasted about 1000 years, indicating a long-term transmission of history with a capacity steadfastness Importance.

To reach these conclusions, scientists conducted geological and archaeological excavations In the Atacama desert. Geological research focused on sedimentary deposits left by the tsunami. dating shells And bits of coal made it possible to fix this event around -1778. Deposit site as well Design From the tsunami made it possible to estimate Magnitude earthquake in mw 9.5 This would have generated a devastating wave 15 to 20 meters high. It is easy to imagine the disastrous impact this tsunami had on the coastal population. Signs of destruction were also observed at many archaeological sites on the coast.

The memory of the disaster has been passed down for nearly 1,000 years

This event marked a major turning point in the organization of the prehistoric societies inhabiting this region, including the massive transformation of the interior or higher regions. The most impressive result is that these inhabitants did not return to live on the coast for 1,000 years. This observation shows that the memory of the tsunami has been passed down from generation to generation, over a period of nearly a thousand years. We also note that in the long term, the population has been resettled in a more careful manner, with the development of housing sites far from the coast or at elevations, at least 20 meters above sea level. The sea, which surprisingly corresponds to the maximum tsunami wave that occurred 1,000 years ago. In what way was this memory of danger conveyed? Scientists do not know. It is certainly oral history, these societies do not yet have a written language.

These findings provide a better understanding of the evolution of the population in this region of the world and their resilience and resilience in the face of a natural disaster of this type. They must also make it possible to better define the risks to the densely populated Chilean coasts.

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