Mayan community was obliterated 1,590 years ago when volcano erupted
Mayan community was obliterated 1,590 years ago when a huge volcano erupted, according to new study that uncovered the timeline using an ice core from Greenland and charred remains from the event
- Radiocarbon measurements date a massive eruption of El Salvador’s Ilopango volcano for the first time, to 431 AD
- The explosion was over 50 times bigger than Mount Saint Helens
- It killed everything within 25 miles and rendered an area twice that size uninhabitable for more than a century
- Analysis of an ice core in Greenland confirmed ash was carried over 4,300 miles
- But the timing is off for it to have led to a strange 18-month era of global cooling
Scientists have pinned down the date of a devastating volcano that rocked the Mayan civilization more than a millennia ago.
It’s long been known that Ilopango volcano, in what is now El Salvador, had a major eruption during the Mayans’ Early Classic Period, between 300 and 600 AD – but a more precise date has eluded researchers until now.
By conducting radiocarbon dating on a charred mahogany tree found in ash deposits, archaeologists have dated the massive explosion to within a few years of 431 AD.
To confirm their findings, researchers used 3D modeling to estimate the eruption plume rose 28 miles into the upper atmosphere.
From there, air currents carried it more than 4,300 miles away, as far as Antarctica.
Analysis of an ice core recovered in Greenland revealed the same chemical makeup, proving their hypothesis correct – the violent eruption occurred 1,590 years ago.
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By conducting radiocarbon dating on a charred mahogany tree found in ash deposits, archaeologists have dated Ilopango volcano’s eruption to within a few years of 431 AD
Today, Ilopango Caldera is a crater lake less than six miles from modern-day San Salvador.
It’s part of El Salvador’s volcanic arc, a chain of 20 active volcanoes that’s one of the most seismically active regions in Central America.
That eruption nearly 1,600 years ago blanketed more than 770,000 square miles of Central America with white ash, earning it the name ‘Tierra Blanca Joven’ – Spanish for ‘young white earth.’
‘It would have been dark over this region for at least a week,’ said lead author Victoria Smith, an archaeologist at Oxford University.
The eruption blanketed more than 770,000 square miles of Central America with white ash, earning it the name ‘Tierra Blanca Joven’ – Spanish for ‘young white earth.’ Researchers estimate its eruption plume rose 28 miles into the upper atmosphere
Tierra Blanca Joven was over 50 times bigger than that of Mount Saint Helens in 1980, Smith added.
The volume of its pyroclastic flows – fast-moving currents of gas, volcanic ash and pumice that can reach 1,830 °F – was ten times that of Mt. Vesuvius when it buried Pompeii.
It killed every living thing within 25 miles and rendered an area twice that size uninhabitable for a century-and-a-half.
‘We think the lack of ceramic production in the general area is because people were not there,’ Smith told Ars Technica.
Tierra Blanca Joven killed everything within 25 miles and rendered an area twice that size uninhabitable for a century-and-a-half. But Mayan civilization survived, having already expanded across Central America by that point
But it didn’t have a severe impact on the rest of Mayan civilization, which had already expanded across Central America by that point.
Research published in 2019 blamed Tierra Blanca Joven for an 18-month period of global cooling around 536 AD, marked by cloudy skies, crop failures and famines as far away as China, reported on by Science Magazine.
But Smith’s research puts the eruption more than a century earlier.
Based on her team’s analysis, Tierra Blanca Joven probably lowered summer temperatures for a few years in the Southern Hemisphere.
HOW CAN RESEARCHERS PREDICT VOLCANIC ERUPTIONS?
According to Eric Dunham, an associate professor of Stanford University’s School of Earth, energy and Environmental Sciences, ‘Volcanoes are complicated and there is currently no universally applicable means of predicting eruption. In all likelihood, there never will be.’
However, there are indicators of increased volcanic activity, which researchers can use to help predict volcanic eruptions.
Researchers can track indicators such as:
- Volcanic infrasound: When the lava lake rises up in the crater of an open vent volcano, a sign of a potential eruption, the pitch or frequency of the sounds generated by the magma tends to increase.
- Seismic activity: Ahead of an eruption, seismic activity in the form of small earthquakes and tremors almost always increases as magma moves through the volcano’s ‘plumbing system’.
- Gas emissions: As magma nears the surface and pressure decreases, gases escape. Sulfur dioxide is one of the main components of volcanic gases, and increasing amounts of it are a sign of increasing amounts of magma near the surface of a volcano.
- Ground deformation: Changes to a volcano’s ground surface (volcano deformation) appear as swelling, sinking, or cracking, which can be caused by magma, gas, or other fluids (usually water) moving underground or by movements in the Earth’s crust due to motion along fault lines. Swelling of a volcano cans signal that magma has accumulated near the surface.
Source: United States Geological Survey