What caused the volcanic tsunami that destroyed a Greek island 373 years ago?

What precipitated the volcanic tsunami that destroyed a Greek island 373 years in the past?

This view from the International Volcano Monitoring System shows the Colombo Crater on the sea floor.
Zoom in / This view from the Worldwide Volcano Monitoring System exhibits the Colombo Crater on the ocean ground.

Santori

In 1650 AD, the Greek island Santorini Destroyed by the eruption of an underwater volcano known as Columbus. Folks first observed the water boiling, altering coloration, and a cone rising from the floor of the ocean. Subsequent got here hurled glowing rocks, fireplace and lightning, thick smoke fumes, falling pumice and ash, earthquakes, and a strong tsunami with waves as much as 20 meters excessive. All this volcanic exercise killed about 70 folks and a whole bunch of livestock.

These particulars are primarily based on modern accounts compiled by a French geologist Ferdinand A. Fouquet in 1879. Now a workforce of German and Greek scientists has mixed this historic data with 3D seismic mapping and pc simulations to find out why a violent volcanic eruption precipitated a tsunami. in line with New paper Revealed within the journal Nature Communications, the tsunami was brought on by a landslide adopted by a volcanic eruption.

Colombo Volcano is situated about 8 kilometers northeast of Santorini Around 1630 BC With disastrous penalties for historic Minoan tradition. Immediately, the volcano homes sulfide and sulfate hydrothermal vents which might be residence to some uncommon species of microorganisms not usually discovered wherever else close to hydrothermal vents. and that is Stay active And doubtlessly harmful: there was a beforehand unknown magma chamber Find out last year It grows at a charge of about 4 million cubic meters yearly. At this charge, the chamber will attain the identical quantity as the quantity of magma ejected within the 1650 eruption inside the subsequent 150 years.

3D seismic dataset of Colombo Volcano.
Zoom in / 3D seismic dataset of Colombo Volcano.

J. Carstens et al., 2023

a 2016 study He concluded that the 1650 tsunami that struck Santorini was probably the results of a big displacement of water brought on by an underwater explosion on September 29 of that 12 months, because the eruption was transitioning between its first section (pushed virtually fully by submarines) and its second section. . However this newest research paints a extra advanced image.

The workforce used the analysis vessel POSEIDON (which has since been decommissioned) to create a 3D picture of the crater, revealing that it was about 500 meters deep and a couple of.5 kilometers huge, proof of a large explosion. Additionally they observed that one facet of the cone was severely deformed, and that a part of the volcano had virtually definitely slid, according to Co-author Gareth Crutchley of the GEOMAR Helmholtz Heart for Ocean Analysis in Kiel. The following step was to conduct pc simulations to match varied potential mechanisms with historic eyewitness accounts.

Simulations confirmed that waves from a volcanic eruption alone might have been as much as 6 meters excessive at a given location, however this conflicts with eyewitness accounts from the identical location that describe a lot greater waves of 20 metres. That simulation additionally confirmed the crest of a wave reaching the coast first, contradicting historic accounts that say the waters first receded at that time earlier than the tsunami surge. Pc simulations of landslide impacts alone didn’t match historic accounts.

It was solely when simulations mixed the explosion and landslide that results per historic information have been produced. Final 12 months’s eruption Hunga Tonga underwater volcano– The strongest since Krakatoa volcanic eruption in 1883– It precipitated a number of tsunamis. The crater has the same form, and the authors recommend {that a} comparable frequent mechanism might trigger these tsunamis as nicely.

Reflection seismic features of the Colombo Monument and its wings
Zoom in / Reflection seismic options of the Colombo Monument and its wings

“Colombo consists partly of pumice stone with steep slopes.” said co-author Jens Carstens, in addition to with the GEOMAR Helmholtz Heart for Ocean Analysis in Kiel. “It isn’t very steady. Through the eruption, which lasted for a number of weeks, lava was consistently spewed out. And under, within the magma chamber, which contained loads of gasoline, there was great stress. When one facet of the volcano exploded because it slid, it The impact is like opening a bottle of champagne: The sudden launch of stress allowed the gasoline within the magma system to broaden, leading to a large explosion.

Colombo and comparable shallow, lively underwater volcanoes are monitored intermittently, however in line with the authors, present monitoring strategies won’t decide up quickly rising deformed flanks weak to landslides just like what occurred with Colombo in 1650. At present unprepared for the threats posed by submarine explosions and slope failures, As evidenced by the sector’s latest collapse in 2018 Children of Krakatoa They wrote: “Hunga Tonga volcano eruption in 2022.” Carstens and others hope to develop new steady monitoring strategies primarily based on their new information to create an early warning system that provides residents extra time to evacuate to security.

Nature Communications, 2023. DOI: 10.1038/s41467-023-42261-y (About digital IDs).

Similar Posts

Leave a Reply

Your email address will not be published. Required fields are marked *