
Human skull on Mars? What did NASA just discover on the red planet
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A curious discovery has captured the attention of both scientists and space enthusiasts. On Mars 's remote slope of Jezero Crater, NASA 's Perseverance rover sent back an image of a rock that resembled a human skull. About the size of a basketball, the rock-like structure is completely different from its dusty surroundings.For some people, it may seem like a cosmic coincidence, but for others, it is another reminder of the Red Planet's mystery and the possibility of life outside Earth.The Perseverance rover is a car-sized robotic spacecraft dispatched by NASA to explore the Jezero Crater on Mars as a key part of the Mars 2020 mission.According to Margaret Deahn, a Ph.D. student at Purdue University and a member of the NASA team, Skull Hill is most likely what's known as a 'float rock.' This means it didn't originate where it currently sits but was transported there by natural forces, likely from an impact crater or volcanic activity.'It could have come from a volcanic outcrop or a distant impact, carried over by ancient Martian winds or water flows,' Deahn explained. Scientists also estimate that as much as 30% of the surface rocks in Jezero Crater may have been displaced over millions of years.Some even suggest that it could be a meteorite, as Mars' thin atmosphere a lot of times fails to burn up the incoming space debris, and NASA's Curiosity rover had found several iron-nickel meteorites in Gale Crater.But in this case, after a closer inspection, Perseverance's SuperCam, which is a laser-powered chemical analyzer, revealed that Skull Hill's composition didn't match that of a typical meteorite.It also suggested that the object is an igneous rock formed from volcanic magma, and the presence of minerals like olivine and pyroxene, which are considered common in volcanic rocks, supports this theory.The pitted and angular surface of the Skull, along with its dark tone, makes it even more interesting. The pits are likely the result of wind erosion or the loss of small rock fragments. Rocks like Skull Hill are time capsules, offering critical clues about the planet's geological history and helping in understanding Mars' past.'Every rock we encounter on Mars is like a page in the planet's unfinished autobiography,' said Dr. Melissa Rice, a planetary geologist at Western Washington University. 'And Skull Hill? It's one of those chapters that makes you stop and think.'The question of whether Mars was ever home to life remains one of the most curious mysteries, and the search continues, with the hope that one day, the Red Planet will reveal its secrets.
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But what exactly had triggered this steady, global beat?The answer lay in a massive natural disaster: on 16 September 2023, more than 25 million cubic metres of rock and ice—a volume large enough to fill 10,000 Olympic swimming pools—collapsed from the mountainside into Dickson Fjord. This triggered a mega-tsunami with waves reaching 650 feet high, about half the height of the Empire State waves surged along the two-mile-long fjord, smashing against cliffs and bouncing back, creating a prolonged sloshing motion known as a seiche. Unlike tsunamis, which travel outward as single giant waves, seiches occur when water oscillates repeatedly in an enclosed space. This ongoing motion produced rhythmic seismic pulses detectable around the are caused by sudden, large displacements of water—usually due to earthquakes, landslides, or volcanic eruptions—and travel as single massive waves. Seiches, however, are standing waves formed in enclosed or semi-enclosed bodies of water, like lakes or fjords. They can be triggered by landslides or strong winds, causing the water to rock back and forth in a steady Dickson Fjord, the narrow, enclosed shape trapped the tsunami energy. The waves couldn't escape, so they kept bouncing, sending low-frequency seismic energy through the Earth's crust for mystery was unraveled thanks to the Surface Water and Ocean Topography (SWOT) satellite, a joint NASA and French space agency mission launched in December 2022. Unlike traditional satellites that scan narrow lines, SWOT uses Ka-band Radar Interferometer (KaRIn) technology to map wide swaths of ocean surface in high SWOT data, researchers observed subtle water elevation changes—slopes of up to two metres—sloshing across the fjord. These shifts matched the oscillations expected from fill gaps, scientists employed machine learning to simulate wave behaviour over time. They also analysed crustal deformation data from sensors thousands of kilometres away, plus weather and tidal records, ruling out other causes like researcher Thomas Monahan, a University of Oxford engineering student, said, 'Climate change is giving rise to new, unseen extremes. These changes are happening fastest in remote areas like the Arctic, where our ability to monitor them has historically been limited.'The underlying cause of the landslide was the rapid melting of Greenland's glaciers. As glacier ice shrinks, it removes the natural support holding mountainsides in place. This weakening triggers massive rock and ice explained, 'Climate change is shifting what is typical on Earth, and it can set unusual events into motion.' Past disasters, like a deadly tsunami in Karrat Fjord in 2017, show how these events can devastate local Fjord lies near popular cruise routes, raising concerns about future risks as Arctic tourism grows. Authorities are now exploring early-warning systems combining satellite data and real-time seismic monitoring to protect people in vulnerable event represents a turning point in how we observe and understand Earth's dynamic processes. Professor Thomas Adcock of Oxford said, 'This study is an example of how the next generation of satellite data can resolve phenomena that have remained a mystery in the past.'He added, 'We will be able to get new insights into ocean extremes such as tsunamis, storm surges, and freak waves. To fully harness these data, we need to innovate using both machine learning and ocean physics.'A Danish military vessel patrolled the fjord three days after the first pulse but observed nothing unusual. This shows how even massive natural events can leave little trace without sophisticated monitoring are now searching through historical seismic data for similar slow, rhythmic pulses. 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an hour ago
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Dickson Fjord's 650-foot mega-tsunami: How a giant wave sent shockwaves worldwide
In September 2023, Greenland's Dickson Fjord experienced a colossal landslide that triggered a 650-foot mega-tsunami, causing the Earth to pulse with rhythmic seismic signals every 90 seconds for nine days. New research using next-generation satellite technology and machine learning has revealed how these waves, called seiches, sloshed back and forth in the fjord, creating global seismic vibrations. The event highlights the hidden impacts of climate change in remote Arctic regions and marks a breakthrough in Earth monitoring technology. Tired of too many ads? Remove Ads Mega-tsunamis rock Greenland's Fjord Seiches vs. Tsunamis: The science behind the waves Tired of too many ads? Remove Ads How advanced satellites and machine learning solved the puzzle Climate Change: The silent driver Tired of too many ads? Remove Ads A breakthrough in Earth monitoring In September 2023, seismic stations worldwide began picking up an unusual, rhythmic signal repeating every 90 seconds. This steady pulse continued for nine days and returned briefly a month later. It was faint, unlike a typical earthquake, but strong enough to register across continents—from Alaska to Australia. Scientists were baffled. No known earthquake, volcanic eruption, or explosion had caused source was traced to the remote Dickson Fjord in East Greenland, a narrow inlet bordered by towering cliffs. But what exactly had triggered this steady, global beat?The answer lay in a massive natural disaster: on 16 September 2023, more than 25 million cubic metres of rock and ice—a volume large enough to fill 10,000 Olympic swimming pools—collapsed from the mountainside into Dickson Fjord. This triggered a mega-tsunami with waves reaching 650 feet high, about half the height of the Empire State waves surged along the two-mile-long fjord, smashing against cliffs and bouncing back, creating a prolonged sloshing motion known as a seiche. Unlike tsunamis, which travel outward as single giant waves, seiches occur when water oscillates repeatedly in an enclosed space. This ongoing motion produced rhythmic seismic pulses detectable around the are caused by sudden, large displacements of water—usually due to earthquakes, landslides, or volcanic eruptions—and travel as single massive waves. Seiches, however, are standing waves formed in enclosed or semi-enclosed bodies of water, like lakes or fjords. They can be triggered by landslides or strong winds, causing the water to rock back and forth in a steady Dickson Fjord, the narrow, enclosed shape trapped the tsunami energy. The waves couldn't escape, so they kept bouncing, sending low-frequency seismic energy through the Earth's crust for mystery was unraveled thanks to the Surface Water and Ocean Topography (SWOT) satellite, a joint NASA and French space agency mission launched in December 2022. Unlike traditional satellites that scan narrow lines, SWOT uses Ka-band Radar Interferometer (KaRIn) technology to map wide swaths of ocean surface in high SWOT data, researchers observed subtle water elevation changes—slopes of up to two metres—sloshing across the fjord. These shifts matched the oscillations expected from fill gaps, scientists employed machine learning to simulate wave behaviour over time. They also analysed crustal deformation data from sensors thousands of kilometres away, plus weather and tidal records, ruling out other causes like researcher Thomas Monahan, a University of Oxford engineering student, said, 'Climate change is giving rise to new, unseen extremes. These changes are happening fastest in remote areas like the Arctic, where our ability to monitor them has historically been limited.'The underlying cause of the landslide was the rapid melting of Greenland's glaciers. As glacier ice shrinks, it removes the natural support holding mountainsides in place. This weakening triggers massive rock and ice explained, 'Climate change is shifting what is typical on Earth, and it can set unusual events into motion.' Past disasters, like a deadly tsunami in Karrat Fjord in 2017, show how these events can devastate local Fjord lies near popular cruise routes, raising concerns about future risks as Arctic tourism grows. Authorities are now exploring early-warning systems combining satellite data and real-time seismic monitoring to protect people in vulnerable event represents a turning point in how we observe and understand Earth's dynamic processes. Professor Thomas Adcock of Oxford said, 'This study is an example of how the next generation of satellite data can resolve phenomena that have remained a mystery in the past.'He added, 'We will be able to get new insights into ocean extremes such as tsunamis, storm surges, and freak waves. To fully harness these data, we need to innovate using both machine learning and ocean physics.'A Danish military vessel patrolled the fjord three days after the first pulse but observed nothing unusual. This shows how even massive natural events can leave little trace without sophisticated monitoring are now searching through historical seismic data for similar slow, rhythmic pulses. Carl Ebeling from UC San Diego said, 'This shows there is stuff out there that we still don't understand and haven't seen before.'Every new discovery will improve forecasts of how landslides, fjord shapes, and water depth interact. The hope is to provide early warnings that could save lives in remote, high-latitude silent, powerful waves in Greenland's fjord prove one thing: the most isolated places on Earth are changing fast—and we must listen carefully to what they tell us.