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Scientists Say The Earth's Core Is Literally Leaking Gold
Scientists Say The Earth's Core Is Literally Leaking Gold

Yahoo

time03-06-2025

  • Business
  • Yahoo

Scientists Say The Earth's Core Is Literally Leaking Gold

"Hearst Magazines and Yahoo may earn commission or revenue on some items through these links." Here's what you'll learn when you read this story: Precious metals are leaking out of Earth's core into the mantle, a new study suggests. Scientists identified a particular isotope of ruthenium (Ru) in volcanic rock samples—a form that typically only occurs in Earth's core. Researchers say that they must conduct further studies to determine whether the 'leak' has happened throughout Earth's existence or if it's a new phenomenon. Gold isn't as rare as you may think—it's just hard to reach. 99.999 percent of Earth's precious metals lay hundreds of miles beneath the surface, trapped inside the planet's molten core. If the transparent distance didn't make accessing gold difficult enough, we're also separated from the ore by (literal) tons of solid rock. Fortunately, Earth is making it easier for us humans. According to a new study published in the journal Nature, Earth's core is 'leaking' gold. Now, don't get too excited—gold isn't spewing out of the ground in cartoon-esque fountains—but the researchers on the study did find evidence that precious metals are oozing out of Earth's core and into the mantle. Unlike the core, the mantle is mostly solid, and makes up most of the planet (84 percent of the Earth's volume to be exact). Comparatively, the mantle also has less of a platinum-group-metal called ruthenium, or Ru. Scientists discovered traces of Ru while studying samples of volcanic rocks from Hawaii and concluded that they must have come from Earth's core. 'When the first results came in, we realized that we had literally struck gold,' first author of the study Nils Messling said in a press release. 'Our data confirmed that material from the core, including gold and other precious metals, is leaking into the Earth's mantle above.' New procedures developed by the University of Göttingen allowed researchers to detect the microscopic markers that indicate the Ru actually came from the molten core. According to the paper, when Earth's core formed 4.5 billion years ago, the Ru came from a different source than the trace amounts of the element that naturally occur in the mantle. The differences in the isotopes are so small, however, that it was previously impossible to distinguish them. On top of procedural revolutions, the study is also notable in that it supports wider geological theories. Evidence from the study affirms the plate tectonics theory that oceanic islands formed from molten material. 'Our findings not only show that the Earth's core is not as isolated as previously assumed,' Matthias Willbold, another author of the study, said in the release. 'We can now also prove that huge volumes of super-heated mantle material–several hundreds of quadrillion metric tonnes of rock–originate at the core-mantle boundary and rise to the Earth's surface to form ocean islands like Hawaii.' As for the future, the researchers expressed that there is still much to learn, particularly when it comes to the timeline of the 'leak.' 'Whether these processes that we observe today have also been operating in the past remains to be proven,' Messling explained. 'Our findings open up an entirely new perspective on the evolution of the inner dynamics of our home planet.' You Might Also Like The Do's and Don'ts of Using Painter's Tape The Best Portable BBQ Grills for Cooking Anywhere Can a Smart Watch Prolong Your Life?

Scientists catch Earth's core leaking gold toward the surface
Scientists catch Earth's core leaking gold toward the surface

Yahoo

time28-05-2025

  • Business
  • Yahoo

Scientists catch Earth's core leaking gold toward the surface

The world's largest stash of gold isn't at Fort Knox: It's locked away in Earth's core. Now, new research from Göttingen University in Germany suggests that some gold might be leaking from the core into the mantle and the crust, bringing it another step closer in the long, and slow, upward journey to the surface. The findings, published this month in the journal Nature, trace the precious metal Ruthenium (Ru) in volcanic rocks from Hawaii back to the core-mantle boundary, which lies more than 3,000 kilometres underground. Most of Earth's gold and other precious metals like platinum and palladium are believed to have sunk into the metallic core during the planet's early, molten days. We can access gold from Earth's crust, but what lies there represents only 1 per cent of the total quantity of gold on the planet. More than 99 per cent of it is thought to be in the core. If that 99 per cent were placed on the surface, there would be enough to blanket all the land on Earth in a half-metre layer of gold. The authors of the new study say tiny differences in isotopes hold clues about when deep-earth elements appear closer to the surface. One isotope, 100Ru, is found in higher concentrations in the core than in the mantle. Using refined techniques, researchers detected high levels of 100Ru in Hawaiian lava samples. 'When the first results came in, we realized that we had literally struck gold!" says Dr. Nils Messling from the university's Department of Geochemistry, in a statement. "Our data confirmed that material from the core, including gold and other precious metals, is leaking into the Earth's mantle above.' The discovery challenges the assumption the planet's core is geochemically sealed off from the surrounding mantle and suggests some of the core's metal-rich contents leak upwards. But don't expect a gold rush anytime soon. Digging 2,900 km down to access the minerals isn't realistic, but the paper does offer new insight into what goes on deep underground. The findings suggest all siderophile elements, i.e., those that prefer to bond with iron and were drawn into the core early in Earth's formation, may be gradually leaking out. That includes ruthenium, gold, platinum, rhodium, and palladium. 'Our findings not only show that the Earth's core is not as isolated as previously assumed,' says Professor Matthias Willbold, also of the Department of Geochemistry, in the same statement. 'We can now also prove that huge volumes of super-heated mantle material – several hundreds of quadrillion metric tonnes of rock – originate at the core-mantle boundary and rise to the Earth's surface to form ocean islands like Hawaii.' This research not only adds to our understanding of Earth's interior but could also reshape what we know about the evolution of other rocky planets across the solar system. Header image: Graphic representation of Earth's shell structure showing the super-heated metallic inner core in the centre, followed by the solid outer core, the rocky mantle and the thin crust towards the surface. New research from the University of Göttingen demonstrates that some precious metal-rich material from the core is leaking into the Earth's mantle above. University of Göttingen/ (OpenAI)

Is Earth's core leaking gold and other precious metals to the surface?
Is Earth's core leaking gold and other precious metals to the surface?

First Post

time27-05-2025

  • Science
  • First Post

Is Earth's core leaking gold and other precious metals to the surface?

A new study in Nature reveals that Earth's core may not be sealed shut after all. German geochemists have discovered traces of core-derived precious metals like ruthenium in volcanic rocks from Hawaii — suggesting gold and other elements may be slowly seeping up from deep within the planet read more A woman and her daughter touch a structural model of the earth's core at Nanjing Geological Museum in Nanjing, Jiangsu province, April 22, 2011. The Chinese characters on the model read "outer core". Representational Image/Reuters Scientists have found robust suggesting that Earth's inner core, long considered completely sealed off, is slowly releasing gold and other precious metals into the layers above. This revelation comes from a detailed isotope study of volcanic rocks, specifically basalt samples from Hawaii, which shows that some of the world's most valuable elements may have originated not just from meteorites or the planet's mantle, but from the very centre of Earth itself. Geochemists from the University of Göttingen in Germany, including Nils Messling and Matthias Willbold, have published their findings in the scientific journal Nature, revealing how specific isotopes act as tracers for material that originated in Earth's metallic core. STORY CONTINUES BELOW THIS AD How Earth's core is seen as a hidden reservoir For decades, scientists have known that the overwhelming majority of Earth's gold — along with elements like platinum, palladium, rhodium and ruthenium — is not found in the crust or even the upper mantle, but locked away in the core, buried beneath nearly 3,000 kilometres of dense rock. This concentration of heavy elements occurred during Earth's early years, over 4.5 billion years ago, when the planet's internal structure began to differentiate. Heavier elements sank toward the centre during a process known as the iron catastrophe, leaving the outer layers comparatively depleted. Also Watch: According to estimates, the quantity of gold sequestered in the core is so vast that, if extracted and spread evenly over the land surface, it could cover every continent with a 50-centimetre-thick layer of gold. Yet, until recently, this immense subterranean reserve was believed to be geologically unreachable and completely cut off from the crust. That assumption has now been upended. How scientists tracked core-derived isotopes in volcanic rock The Göttingen researchers focused on analysing isotopic compositions in rocks formed from deep-Earth magmatic activity. They targeted ruthenium, a rare and heavy element that exhibits subtle isotopic differences depending on its source. These differences had previously been too minute to distinguish. But by refining their laboratory techniques, the team was able to detect and compare ruthenium isotopes with unprecedented precision. Using samples from basaltic lava flows in the Hawaiian islands — an area known for volcanic activity stemming from deep mantle plumes — the researchers discovered an elevated concentration of the isotope ruthenium-100. STORY CONTINUES BELOW THIS AD This variant is consistent with material originating from Earth's core, as opposed to the surface or upper mantle. 'Our data confirmed that material from the core, including gold and other precious metals, is leaking into the Earth's mantle above,' said Nils Messling, one of the lead authors of the study. 'When the first results came in, we realised that we had literally struck gold!' The core-derived signature in the volcanic rock was not limited to ruthenium. It suggests that other siderophile elements — those with an affinity for iron and which bonded with it in the early, molten Earth — may also be part of the upward movement from core to mantle, and eventually, to the crust. How core material reaches the surface The study provides compelling evidence that deep mantle upwellings — also called mantle plumes — transport material from near the core-mantle boundary to the surface. These massive columns of superheated rock rise through the mantle and erupt through oceanic crust to form volcanic islands such as those in Hawaii. 'We can now also prove that huge volumes of superheated mantle material—several hundred quadrillion metric tons of rock—originate at the core-mantle boundary and rise to the Earth's surface to form ocean islands like Hawaii,' said study co-author Matthias Willbold. STORY CONTINUES BELOW THIS AD Also Watch: The volume and force of this process are immense, although it happens over geological timescales spanning millions of years. The volcanic rocks that emerge during these eruptions carry chemical and isotopic clues from the depths, making them natural record-keepers of Earth's internal dynamics. What this means for future research The discovery opens new avenues for understanding how Earth's internal systems have evolved over billions of years. Prior to this discovery, the prevailing understanding among Earth scientists was that the planet's core, encased beneath the solid silicate mantle and crust, was an isolated and chemically inert reservoir. The new research not only confirms that elements like ruthenium and possibly gold are slowly migrating upward, but it also introduces the use of isotopic 'tracers' to monitor and quantify this migration in future studies. Ruthenium, in particular, may serve as a powerful tool for understanding the interactions between Earth's layers. 'Precious metals such as ruthenium are highly concentrated in the metallic core but extremely depleted in the silicate mantle,' the researchers wrote in their study. While many of Earth's surface metals were believed to have arrived via meteorite bombardment during the early years of the solar system, this study shows that at least some of those metals may have originated from within the planet itself. STORY CONTINUES BELOW THIS AD 'Our findings open up an entirely new perspective on the evolution of the inner dynamics of our home planet,' the researchers concluded. While practical access to these deeply buried resources remains impossible with current technology, the scientific insight gained from these findings may influence everything from geochemistry to planetary science. This revelation also has implications beyond Earth. If core leakage of precious metals is possible here, similar processes may occur on other rocky planets. Though no gold rush will result from this research, its value lies in the new understanding it offers about Earth's inner mechanics. Also Watch: With input from agencies

Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks
Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks

Yahoo

time27-05-2025

  • Science
  • Yahoo

Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks

A German university, Göttingen University, has literally "struck gold" in recent findings from volcanic rocks. A new study of these volcanic rocks from Hawaii, that leaked out from deep under the lithosphere, contained various precious metals. Dr. Nils Messling of the Göttingen University's Department of Geochemistry said in a news release they were surprised when the test results came in. "When the first results came in, we realized that we had literally struck gold! Our data confirmed that material from the core, including gold and other precious metals, is leaking into the Earth's mantle above," Messling said. Largest Gold Deposit In The World Worth $83 Billion Found In China Approximately 99% of the Earth's gold is buried deep in the Earth's Metallic Core, far out of humankind's reach. Read On The Fox News App The gold is currently buried about 1,800 miles deep in the core. The discovery of this ruthenium, which was formed and locked down with gold, might be a telling sign that these volcanic rocks are coming from deep within the Earth. Hawaii's Kilauea Volcano Erupts With 1,000-Foot 'Lava Fountaining' "Our findings not only show that the Earth's core is not as isolated as previously assumed. We can now also prove that huge volumes of super-heated mantle material – several hundreds of quadrillion metric tonnes of rock – originate at the core-mantle boundary and rise to the Earth's surface to form ocean islands like Hawaii," said Professor Matthias Willbold in a news release. There is a way to test for isotopes of ruthenium, especially when differences are small variations of the same element. The isotopes of ruthenium in the Earth's core are slightly different from those on the surface, with the difference being too small to really detect. However, new procedures developed by researchers at the University of Göttingen have made it possible. "Whether these processes that we observe today have also been operating in the past remains to be proven. Our findings open up an entirely new perspective on the evolution of the inner dynamics of our home planet," Messling said in a statement. With these precious metals beginning to leak to the Earth's surface, it could suggest that the supplies of gold and others important for renewable energy came from the Earth's article source: Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks

Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks
Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks

Fox News

time27-05-2025

  • Science
  • Fox News

Scientists 'strike gold' in shocking discovery from Hawaiian volcanic rocks

A German university, Göttingen University, has literally "struck gold" in recent findings from volcanic rocks. A new study of these volcanic rocks from Hawaii, that leaked out from deep under the lithosphere, contained various precious metals. Dr. Nils Messling of the Göttingen University's Department of Geochemistry said in a news release they were surprised when the test results came in. "When the first results came in, we realized that we had literally struck gold! Our data confirmed that material from the core, including gold and other precious metals, is leaking into the Earth's mantle above," Messling said. Approximately 99% of the Earth's gold is buried deep in the Earth's Metallic Core, far out of humankind's reach. The gold is currently buried about 1,800 miles deep in the core. The discovery of this ruthenium, which was formed and locked down with gold, might be a telling sign that these volcanic rocks are coming from deep within the Earth. "Our findings not only show that the Earth's core is not as isolated as previously assumed. We can now also prove that huge volumes of super-heated mantle material – several hundreds of quadrillion metric tonnes of rock – originate at the core-mantle boundary and rise to the Earth's surface to form ocean islands like Hawaii," said Professor Matthias Willbold in a news release. There is a way to test for isotopes of ruthenium, especially when differences are small variations of the same element. The isotopes of ruthenium in the Earth's core are slightly different from those on the surface, with the difference being too small to really detect. However, new procedures developed by researchers at the University of Göttingen have made it possible. "Whether these processes that we observe today have also been operating in the past remains to be proven. Our findings open up an entirely new perspective on the evolution of the inner dynamics of our home planet," Messling said in a statement. With these precious metals beginning to leak to the Earth's surface, it could suggest that the supplies of gold and others important for renewable energy came from the Earth's core.

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