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A Pompeii-Like Eruption Buried This Landscape 22 Million Years Ago—Scientists Just Discovered What Lies Beneath

16 September 2026 at 15:06

The Americas experienced their own Vesuvius-style volcanic eruption 21.9 million years ago, devastating a portion of Chile worse than Pompeii.

A new study in Science Advances highlights the work of University College London Earth Sciences researchers analyzing a mountain of ancient volcanic rock covering an area six times the size of the Chilean capital, Santiago. 

The Lauca Caldera erupted to cover the area in molten ignimbrite rock up to a kilometer deep. That ancient volcanic hellscape buried the region’s terrain but, ironically, preserved it from typical erosion, providing important clues for modern climate researchers.

Modeling Volcanic Activity

“This landscape was buried by a giant volcanic eruption – a little like Pompeii, but on a vastly larger scale,” said lead author Dr Byron Adams, based at UCL Earth Sciences. “Instead of covering a town, hot mixtures of volcanic ash, rock fragments, and gas swept across an entire landscape, engulfing the terrain beneath them.”

Using detailed computer models, the UCL Earth Sciences team produced hundreds of possible landscapes to explore what the region may have once looked like. Detailed data on how rivers cut through landscapes to form mountain ranges informed predictions of what lies beneath the massive ignimbrite deposits. The researchers concluded that a low-relief landscape, such as foothills, most likely existed there at the time.

“Pompeii shows how volcanic eruptions can freeze a moment in human history. This study shows that much larger eruptions can also freeze moments in Earth history, burying whole landscapes beneath volcanic deposits and preserving clues to how mountains were being built before the eruption,” Adams said.

“We cannot dig down to see the buried landscape, but we can use the shape of the volcanic blanket and what we know about how rivers shape mountains to infer what is hidden beneath it.”

The Volcanic Andes

The findings indicate that this portion of the Andes, the world’s longest continental mountain range, rose very slowly, by only about an inch per century. At a faster rate, the landscape beneath the volcanic deposits would not fit the researchers’ models, and the slopes would have been much steeper.

The work provides new evidence in a longstanding debate among geologists over whether the Andes rose rapidly in the last few million years or developed more gradually over a much longer period. Earlier mineral analyses of the Andean range produced similar estimates based on records of temperature changes preserved in the rocks as they cooled while moving toward the planet’s surface.

“This approach gives us a new way to look back at Earth’s history. Current methods to estimate the speed at which mountains build look at chemical ‘clocks’ in the rock, but these are limited to specific moments in time. Our method can estimate rock uplift over a much longer period,” Dr. Adams said. “In this case, we estimate it would have taken millions of years to produce the subdued landscape we infer prior to the eruption.”

Other mountain ranges around the world, such as the Himalayas, can move even faster, rising several millimeters or even centimeters each year.

Climate Implications

While the team’s work covers only the middle of the Andes’ history, it still provides interesting support for the slow-movement hypothesis. For years, researchers have worked to understand how the Andes developed, as they strongly influence global and regional climate. 

By better understanding the Andes, climatologists have a more complete data set to piece together the complex problem of global climate change.

“What’s particularly exciting about this study is that it gives us a new way of piecing together that history, concluded co-author Dr Frances Cooper, also based at UCL Earth Sciences. “The same approach could be applied to volcanic deposits elsewhere in the world, helping us reconstruct landscapes buried for millions of years.”

The paper, “Landscapes Buried Beneath Large-Volume Ignimbrites Reveal Preeruptive Uplift Rates,” appeared in Science Advances on September 11, 2026.

Ryan Whalen covers science and technology for The Debrief. He holds an MA in History and a Master of Library and Information Science with a certificate in Data Science. He can be contacted at ryan@thedebrief.org, and follow him on Twitter @mdntwvlf.

What Caused Antarctica to Freeze Millions of Years Ago? New Clues Could Finally Solve This Longstanding Climate Mystery

4 September 2026 at 17:32

New clues to the formation of our planet’s oldest and largest ice sheet could help resolve a longstanding enigma about the southernmost continent.

Around 34 million years ago, Antarctica’s ice sheet began to take shape during a period when global temperatures were predominantly warmer than they are at present. The exact reason why such a large portion of Earth’s water would be subsumed into a massive ice sheet under such conditions has long perplexed researchers.

Now, a new study published in the journal Science suggests that clues to the mystery may exist beneath the ice itself, according to researchers who point to geological evidence that could help explain what led to the formation of Antarctica’s glaciers during a comparatively warm period in our planet’s history.

Clues to Why a Continent Froze

The East Antarctic Ice Sheet (EAIS) holds enough frozen water that it could raise sea levels around the world by more than 50 meters if a sudden, total melting event were ever to occur. Fortunately, scientists don’t anticipate that happening any time soon, although questions over what caused the formation of the largest mass of ice on our planet have remained one of the most predominant mysteries about Antarctica’s ancient history.

Based on geological evidence and paleo-climatological proxy data, the ice sheet’s formation occurred near the transition between the Eocene and Oligocene eras around 34 million years ago, marking a significant step along our planet’s path toward the cooler conditions that prevail today, even amid anthropogenic factors that contribute to ongoing climate changes.

As far as the causes behind this, scientists have long pointed to a reduction in atmospheric carbon dioxide as one potential driver of glaciation in Antarctica. However, this explanation also leads to questions: namely, that if falling CO2 and global cooling are believed to be the main factors behind the formation of Antarctica’s ice, then similar freezing should have occurred close to the North Pole as well.

Curiously, evidence suggests that glaciation in Earth’s northernmost regions didn’t begin catching up to its southern counterpart for another 20 to 25 million years. But what might account for this?

An Ancient Climate Missing Link

The new research, led by scientists at the University of Southampton in collaboration with an international team of researchers from Durham University and several other institutions, points to Antarctica’s changing landscape as a likely missing piece to this ancient puzzle.

“Antarctica’s land surface was gradually lifted to the point where ice could gain a permanent foothold, even while the surrounding polar oceans as well as global temperatures remained surprisingly warm,” said Thomas Gernon, a Professor of Earth Science at the University of Southampton and the study’s lead author.

By employing models that helped the team map the evolution of the Antarctic landscape, they were able to successfully reconstruct the ancient geological processes going all the way back to the original breakup between Africa and Antarctica that reshaped East Antarctica. This continental breakup led to the formation of a coastal escarpment in the region identified today as Dronning Maud Land, where an elevated plateau rose to nearly two kilometers, and extended close to 2,000 kilometers inland.

Over the 100 million years that followed, a wave of uplift and erosion gradually migrated inland toward Antarctica’s Gamburtsev Mountains, a process which would recur again during the Eocene, further elevating the region and increasing the amount of ancient Antarctica’s landmass that was above the permanent snow line, all of which occurred roughly 15 million years before mass-scale glaciation would begin on the continent.

Based on the team’s models, these major changes to the landscape shifted East Antarctica above the threshold where ice-sheet growth could begin occurring, the onset of which began around 45 million years ago.

Combined Factors Behind Antarctica’s Freeze

Another factor the team identified involves how the large-scale glaciation also caused more sunlight to be reflected away from Earth due to the icy surface’s light coloration, a process known as albedo feedback. The team believes this reflected sunlight may have contributed to as much as an additional degree Celsius of total global cooling.

That cooling alone, the researchers note, would not have been enough to cause widespread glaciation across the Northern Hemisphere, which generally features lower elevations.

Overall, the findings do indicate that Earth’s transition into an icehouse wasn’t something that was driven solely by climate. Instead, what seems most likely is that slow geological transformations occurring over many millions of years were likely to have been a primary contributor to this process, raising Antarctica’s landscape enough to facilitate ice sheet formation, and revealing how the evolution of landscapes can ultimately reshape the climate of an entire planet.

The recent study, “Continental breakup–driven uplift instigated East Antarctic Ice Sheet formation,” appeared in the journal Science.

Micah Hanks is the Editor-in-Chief and Co-Founder of The Debrief. A longtime reporter on science, defense, and technology with a focus on space and astronomy, he can be reached at micah@thedebrief.org. Follow him on X @MicahHanks, and at micahhanks.com.

Researchers Create OnlyFans for Marmots to Bridge Funding Gap

28 July 2026 at 23:58
Daniel Blumstein, a professor of ecology and evolutionary biology at U.C.L.A., faced a funding issue amid federal cuts to scientific research. To raise money for its marmot research, his team started “OnlyMarms,” a free, G-rated account of cute videos that collects money through tips.

“This is Far from an Ordinary Burial”: Archaeologists Have Made Rare Discoveries in an ‘Elite’ Siberian Grave

17 June 2026 at 14:03

A burial site uncovered by archaeologists in southern Siberia has revealed a series of unusual discoveries, which include ritually broken artifacts surrounding human and horse remains.

The burial site was uncovered in the Sayan Mountains and was discovered during a survey in advance of railway construction planned for the area. Archaeologists believe that the grave dates to the tenth century.

Originally uncovered in 2014, excavations at the site of the unusual grave and several others found nearby have been ongoing, revealing discoveries that researchers say are unusual for the period and location.

“It is quite clear that this is far from an ordinary burial,” according to Andrey Poliakov, a researcher with the Russian Academy of Sciences and one of the co-authors of a new study detailing the findings, which appeared in Bulletin of Novosibirsk State University, Series: History, Philology.

Curious Discoveries in a Siberian Grave

Among the unusual discoveries in the Siberian grave were human remains—those belonging to a woman, as well as a newborn child—and animal remains belonging to a horse, including the creature’s skull, skin, and limbs, and a spine that belonged to a sheep.

The woman’s remains were also accompanied by several artifacts, which included bronze earrings, a spindle whorl crafted from stone, and an iron knife. Also associated with the woman’s remains was a mirror, which archaeologists believe may have been intentionally broken for ritual purposes—a practice maintained by many ancient cultures throughout the world.

Siberian elite burial
The woman’s remains at the burial site in the Sayan Mountains revealed a range of artifacts, many of which were dated to earlier times, suggestive of heirlooms that may represent an “elite” burial (Image Credit: Press Service of the Institute of the History of Material Culture of the Russian Academy of Sciences)

Eastern Connections

Also of interest was the design of the mirror, which features carvings of a vine that winds along the artifact and clusters of grapes. The research team believes this could indicate that this artifact, and possibly some of the others found in the grave, may have originated from China.

Additionally, the researchers report that items associated with the remains of the horse contained within the burial site are associated with older periods, which would have made them antiques at the time they were included within the grave. Another example of artifacts with possible eastern origins includes a stirrup, which features decorations that bear resemblance to ancient art found in China and India.

Such stirrups were often employed by nomads who once dwelt on the Eurasian Steppe, and featured on the left side of their saddles—a position which archaeologists also believe may have held ritual significance.

An Elite Burial from the 10th Century

According to the researchers in their study, “The entire set of items constitutes a complete set of riding horse equipment,” which they say has “an archaic appearance and could be preserved for a long time as ‘family heirlooms’.”

The researchers add that such items were particularly popular in ancient nomadic society along the Eurasian Steppe and were viewed “as an indicator of social prestige” during the 8th and 9th centuries.

The unusual collection of artifacts within the grave was considered a rare find for this region, although further interpretation about the remains of the woman and the infant, which may had been her child, may be required.

The paper, “Riding Horse Equipment from a Medieval Burial on the Idzhim River in the Usinskaya Basin,” by Andrey Poliakov and colleagues, appeared in Bulletin of Novosibirsk State University, Series: History, Philology.

Micah Hanks is the Editor-in-Chief and Co-Founder of The Debrief. A longtime reporter on science, defense, and technology with a focus on space and astronomy, he can be reached at micah@thedebrief.org. Follow him on X @MicahHanks, and at micahhanks.com.

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