The purpose of this blog is the creation of an open, international, independent and free forum, where every UFO-researcher can publish the results of his/her research. The languagues, used for this blog, are Dutch, English and French.You can find the articles of a collegue by selecting his category. Each author stays resposable for the continue of his articles. As blogmaster I have the right to refuse an addition or an article, when it attacks other collegues or UFO-groupes.
Druk op onderstaande knop om te reageren in mijn forum
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Deze blog is opgedragen aan mijn overleden echtgenote Lucienne.
In 2012 verloor ze haar moedige strijd tegen kanker!
In 2011 startte ik deze blog, omdat ik niet mocht stoppen met mijn UFO-onderzoek.
BEDANKT!!!
Een interessant adres?
UFO'S of UAP'S, ASTRONOMIE, RUIMTEVAART, ARCHEOLOGIE, OUDHEIDKUNDE, SF-SNUFJES EN ANDERE ESOTERISCHE WETENSCHAPPEN - DE ALLERLAATSTE NIEUWTJES
UFO's of UAP'S in België en de rest van de wereld Ontdek de Fascinerende Wereld van UFO's en UAP's: Jouw Bron voor Onthullende Informatie!
Ben jij ook gefascineerd door het onbekende? Wil je meer weten over UFO's en UAP's, niet alleen in België, maar over de hele wereld? Dan ben je op de juiste plek!
België: Het Kloppend Hart van UFO-onderzoek
In België is BUFON (Belgisch UFO-Netwerk) dé autoriteit op het gebied van UFO-onderzoek. Voor betrouwbare en objectieve informatie over deze intrigerende fenomenen, bezoek je zeker onze Facebook-pagina en deze blog. Maar dat is nog niet alles! Ontdek ook het Belgisch UFO-meldpunt en Caelestia, twee organisaties die diepgaand onderzoek verrichten, al zijn ze soms kritisch of sceptisch.
Nederland: Een Schat aan Informatie
Voor onze Nederlandse buren is er de schitterende website www.ufowijzer.nl, beheerd door Paul Harmans. Deze site biedt een schat aan informatie en artikelen die je niet wilt missen!
Internationaal: MUFON - De Wereldwijde Autoriteit
Neem ook een kijkje bij MUFON (Mutual UFO Network Inc.), een gerenommeerde Amerikaanse UFO-vereniging met afdelingen in de VS en wereldwijd. MUFON is toegewijd aan de wetenschappelijke en analytische studie van het UFO-fenomeen, en hun maandelijkse tijdschrift, The MUFON UFO-Journal, is een must-read voor elke UFO-enthousiasteling. Bezoek hun website op www.mufon.com voor meer informatie.
Samenwerking en Toekomstvisie
Sinds 1 februari 2020 is Pieter niet alleen ex-president van BUFON, maar ook de voormalige nationale directeur van MUFON in Vlaanderen en Nederland. Dit creëert een sterke samenwerking met de Franse MUFON Reseau MUFON/EUROP, wat ons in staat stelt om nog meer waardevolle inzichten te delen.
Let op: Nepprofielen en Nieuwe Groeperingen
Pas op voor een nieuwe groepering die zich ook BUFON noemt, maar geen enkele connectie heeft met onze gevestigde organisatie. Hoewel zij de naam geregistreerd hebben, kunnen ze het rijke verleden en de expertise van onze groep niet evenaren. We wensen hen veel succes, maar we blijven de autoriteit in UFO-onderzoek!
Blijf Op De Hoogte!
Wil jij de laatste nieuwtjes over UFO's, ruimtevaart, archeologie, en meer? Volg ons dan en duik samen met ons in de fascinerende wereld van het onbekende! Sluit je aan bij de gemeenschap van nieuwsgierige geesten die net als jij verlangen naar antwoorden en avonturen in de sterren!
Heb je vragen of wil je meer weten? Aarzel dan niet om contact met ons op te nemen! Samen ontrafelen we het mysterie van de lucht en daarbuiten.
13-01-2026
New Evidence That An Ancient Martian Ocean Covered Half The Planet
New Evidence That An Ancient Martian Ocean Covered Half The Planet
These images highlight three scarp-fronted deposits in a segment of Valles Marineris on Mars. These features are nearly identical to river deltas on Earth, and add to the growing body of evidence showing that ancient Mars was wet and warm, with liquid water flowing on its surface. Image Credit: Argadestya et al. 2026, NPJ Space Exploration/MOLA
Bit by bit, scientists are piecing together Mars' climate history. Thanks to orbiters armed with powerful cameras and rovers carrying suites of scientific instruments, the red planet's history is becoming clearer year-by-year. In the past decade or so, evidence of Mars' ancient habitability is becoming more and more convincing.
In order to be habitable, Mars had to be both warmer and wetter than it is now. There are two broad types of evidence that show that's exactly what it was: One is the existence of minerals that only form in the presence of water, and the other is in landforms created by water. New evidence in NPJ Space Exploration highlights the presence of scarp-fronted deposits in Valles Marineris, features very similar to river deltas here on Earth.
"The structures that we were able to identify in the images are clearly the mouth of a river into an ocean." - Fritz Schlunegger, University of Bern.
Valles Marineris is an extremely large tectonic crack in the Martian crust, and the largest canyon system in the Solar System. Along with Olympus Mons, it's one of Mars' defining features. This research is focused on the southeast part of Coprates Chasma, a massive sub-canyon that's a central part of Valles Marineris.
"Information on water-lain deposits on Mars provides a key contribution to the understanding of the planet’s geologic history and its past environmental conditions, particularly considering the potential for past habitability," the authors write. "Consequently, major scientific efforts have been undertaken to reconstruct the geological history of Mars by documenting the occurrence of water," they write, emphasizing what many Universe Today readers are already aware of.
The researchers used images from multiple orbital cameras: CTX and HiRISE on NASA's Mars Reconnaissance Orbiter, and CaSSIS on the ESA/Roscosmos Trace Gas Orbiter. They also worked with Digital Elevation Models (DEM) based on CaSSIS, Mars Express' High-Resolution Stereo Camera, and the Mars Orbital Laser Altimeter (MOLA) on the now defunct Mars Global Surveyor.
*These figures show the location of the research area in Southeast Coprates Chasma. The red quadrangle in (A) shows the extent of the identified SFDs. The dark blue and yellow rectangles in (B) depict the areas for which HiRISE and CaSSIS images are available, respectively. Basemap image (B): Global CTX V1 overlain with MOLA – HRSC Global DEM V2. Pl= Plateau, Pr= Promontory, and VMD= Valles Marineris Depression.
Image Credit: Argadestya et al. 2026*
They used all this data to examine the "geomorphology of the promontory and the sedimentology of scarp-fronted deposits (SFDs) in Southeast Coprates Chasma," the authors write.
"In the promontory, we find a network of branched channels bordered by screes and bedrock along the drainage divides, indicating a fluvial origin," the researchers explain. "The SFDs, occurring at the downstream end of the promontory, display convex break-in-slopes, separating a flat surface with a radial drainage network from a steep front downstream." The authors say that they interpret these features to be fan-deltas with their sources in the promontory, and that they're records of an ancient high water mark.
Previous research suggested that this was the case, but it lacked the high-resolution DEMs that these authors have at their disposal. According to these results, the SFDs are where a river drained into an ocean and are evidence of an ancient coastline.
"The unique high-resolution satellite images of Mars have enabled us to study the Martian landscape in great detail by surveying and mapping," said lead author Argadestya in a press release.
*(A) shows where three SFDs are located along the northern margin of the promontory in Southeast Coprates Chasma. The dashed black line indicates the boundary of the deposits. The subsequent panels show them in greater detail. The red lines show their rough boundaries, and the white dots show their apexes.
Image Credit: Argadestya et al. 2026*
"CaSSIS has been providing high-resolution color images of the surface of Mars since April 2018," said Nicolas Tomas, Professor at the Department of Space Research & Planetary Sciences (WP) at the University of Bern. "The images are regularly used in scientific studies. I am personally very pleased that the images have now also been used in a geomorphological study by the Institute of Geological Sciences," added Thomas, who provided leadership for the development of the CaSSIS camera.
"When measuring and mapping the Martian images, I was able to recognize mountains and valleys that resemble a mountainous landscape on Earth. However, I was particularly impressed by the deltas that I discovered at the edge of one of the mountains," said Argadestya. SFDs are like river deltas, where fan-shaped deposits of sediments form where a river empties into a body of standing water.
"Delta structures develop where rivers debouch into oceans, as we know from numerous examples on Earth," explained study co-author Fritz Schlunegger, Professor of Exogenous Geology at the Institute of Geological Sciences at the University of Bern. "The structures that we were able to identify in the images are clearly the mouth of a river into an ocean," Schlunegger continues.
*This image shows tributary channels identified in the northward facing promontory of the Southeast Coprates Chasma. The Strahler order in the inset box shows the stream size hierarchy.
Image Credit: Argadestya et al. 2026*
The SFDs are all at about the same elevation in Valles Marineris, and in previous research on the northern lowlands, an important detail. The bulk of research shows they were deposited between the Late Hesperian period and the Early Amazonian period. The Hesperian spanned from 3.7 billion to 3 billion years ago, and the Amazonian period spans from about 3 billion years ago to the current age. "We consider this as the time with the largest availability of surface water on Mars," the authors write.
Multiple studies have shown that ancient Mars had a massive, perhaps global ocean. This study adds to that weight of evidence by providing clear evidence of ancient coastlines.
"We are not the first to postulate the existence and size of the ocean," Schlunegger said. "However, earlier claims were based on less precise data and partly on indirect arguments. Our reconstruction of the sea level, on the other hand, is based on clear evidence for such a coastline, as we were able to use high-resolution images."
*This is an oblique view of a 3D Digital Elevation Model from CaSSIS showing more detail in SFD A. The -3750 and -3650m elevation contours are shown in red dashed lines, indicating the high-water mark of Mars' ancient ocean.
Image Credit: Argadestya et al. 2026*
The three SFDs in Coprates Chasma aren't the only ancient fan deposits on Mars. There are also some in Capri Chasma, Chryse Chaos, and Hydraotes Chaos. This evidence of an ancient paleoshoreline indicates that an ocean reached the same high level from Valles Marineris to the Northern Lowland.
*These panels show where an ancient paleoshoreline existed on Mars. (A) shows the westward extension of the inferred paleoshoreline (orange line) identified in the study area (red rectangle) across the Valles Marineris depression into Chryse Chaos, a transitory region between the Southern highlands and the Northern lowlands on Mars. B,C, and D, show more detail for the three SFDs in the study and how they fit in.
Image Credit: Argadestya et al. 2026*
"With our study, we were able to provide evidence for the deepest and largest former ocean on Mars to date – an ocean that stretched across the northern hemisphere of the planet," said Argadestya.
"In conclusion, the SFDs at the foothills of the Promontory of Southeast Coprates Chasma reflects a period (boundary between the Late Hesperian and the Early Amazonian) with the highest water availability on Mars," the authors write. "We thus consider that our findings on the environmental stage during the Late Hesperian to Early Amazonian will have implications for research on the evidence for potential life on Mars."
NSF–DOE Vera C. Rubin Observatory/NOIRLab/SLAC/AURA/P. Marenfeld
Using early data from the Vera C. Rubin Observatory, which is set to kick off full operations later this spring, an international team of astronomers has discovered an asteroid that spins so fast, it should’ve torn itself apart.
The unusual cosmic lump — dubbed 2025 MN45, 2,300 feet in diameter and located in the Main Asteroid Belt between the orbits of Mars and Jupiter — completes a full rotation every minute and 53 seconds, as detailed in a new paper published in The Astrophysical Journal Letters.
While that may not sound like all that fast at first blush, it’s an astonishing feat considering the object’s sheer bulk. The centrifugal forces involved should’ve already overcome its estimated structural integrity, the researchers found, especially if it were a “rubble pile” made up of smaller rocks, like many other asteroids in the Main Belt.
It’s an especially surprising finding, considering that most distant asteroids were thought to be spinning at much slower rates, as Science Alert points out.
“For objects in the main asteroid belt, the fast-rotation limit to avoid being fragmented is 2.2 hours; asteroids spinning faster than this must be structurally strong to remain intact,” the paper reads. “The faster an asteroid spins above this limit, and the larger its size, the stronger the material it must be made from.”
The team used data collected during the Rubin Observatory’s commissioning phase in the spring of last year to discover 2025 MN45, one of three “ultrafast rotators” that complete a full rotation in less than five minutes. They also found 16 “superfast” rotators with periods between 13 minutes and 2.2 hours. All 19 are larger in diameter than the length of an American football field.
“Clearly, this asteroid must be made of material that has very high strength in order to keep it in one piece as it spins so rapidly,” said Sarah Greenstreet, study lead and assistant astronomer at the National Science Foundation National Optical-Infrared Astronomy Research Laboratory (NOIRLab), in a statement. “We calculate that it would need a cohesive strength similar to that of solid rock.”
“This is somewhat surprising since most asteroids are believed to be what we call ‘rubble pile’ asteroids, which means they are made of many, many small pieces of rock and debris that coalesced under gravity during Solar System formation or subsequent collisions,” she added.
Asteroids beyond the orbit of Mars are very faint and extremely hard to spot. But thanks to the Rubin Observatory’s extremely light-sensitive sensors, the team was able to discover the most distant fast rotators ever spotted.
It’s the first peer-reviewed study that’s based on data from the observatory, and a sure sign that many more discoveries from it are still to come.
“As this study demonstrates, even in early commissioning, Rubin is successfully allowing us to study a population of relatively small, very-rapidly-rotating main-belt asteroids that hadn’t been reachable before,” Greenstreet said.
The Gateway, NASA’s upcoming lunar space station, is one step closer to reality as engineers have successfully powered on its solar electric propulsion system, a spacecraft engine designed to orbit and maneuver around the Moon. This achievement marks a major milestone in NASA’s Artemis program, which aims to establish a sustainable human presence on the lunar surface and prepare for future missions to Mars.
Building The Power And Propulsion Element
At the heart of the Gateway lies the Power and Propulsion Element (PPE), developed under the supervision of NASA’s Glenn Research Center in Cleveland, Ohio. Construction and assembly are led by Lanteris Space Systems in Palo Alto, California, where teams have integrated the spacecraft’s main electrical system within protective panels. This ensures the hardware can withstand the harsh environment of deep space.
Once fully operational, the PPE will generate up to 60 kilowatts of electricity,enough to supply power for communications, navigation, and orbital adjustments. The engine’s advanced solar electric propulsion allows for continuous, efficient thrust powered by sunlight, offering an innovative alternative to traditional chemical propulsion.
The system’s propulsion capability is built around three 12-kilowatt thrusters developed by L3Harris and four 6-kilowatt BHT-6000 thrusters by Busek. Together, these thrusters provide the necessary maneuverability to maintain the Gateway’s orbit and reposition it as needed for lunar missions. Redwire, another NASA partner, is responsible for the roll-out solar arrays, lightweight, flexible panels that convert sunlight into electrical energy.
This hardware will power not only the Gateway’s core functions but also its visiting spacecraft and future science payloads, forming the energetic backbone of NASA’s next-generation lunar operations.
The Gateway’s Role In NASA’s Artemis Program
The Gateway is a cornerstone of NASA’s Artemis program, which aims to return astronauts to the lunar surface for the first time since Apollo 17. Unlike the International Space Station, the Gateway will not be permanently crewed. Instead, it will serve as a modular outpost, orbiting the Moon in a highly stable near-rectilinear halo orbit (NRHO).
This orbit provides ideal access to both the lunar surface and deep space, making it an essential platform for testing life-support systems, radiation protection, and advanced propulsion technologies. Astronauts visiting the Gateway will conduct scientific experiments, prepare landers for surface missions, and evaluate long-duration spaceflight conditions, all critical for future crewed missions to Mars.
NASA envisions Gateway as an international collaboration, involving key contributions from ESA (European Space Agency), JAXA (Japan Aerospace Exploration Agency), and CSA (Canadian Space Agency). Each partner will deliver specialized modules, robotics, and technology to create a truly global platform for exploration.
Engineering A Sustainable Future Beyond Earth
NASA’s decision to rely on solar electric propulsion for the Gateway is both a technological and environmental breakthrough. Unlike conventional rockets, which burn large quantities of fuel in short bursts, this system produces continuous, gentle thrust using electricity derived from sunlight. Over time, it can achieve impressive velocities with minimal resource consumption, an essential feature for long-duration missions far from Earth.
The Gateway will also act as a proving ground for autonomous operations, as it will often function without a human crew onboard. This autonomy will be vital for deep-space missions where communication delays make real-time control impossible. The spacecraft’s design prioritizes efficiency, durability, and adaptability, ensuring it can operate safely and independently in lunar orbit for years at a time.
Through its partnership with Lanteris, L3Harris, Busek, and Redwire, NASA is cultivating a powerful ecosystem of innovation that bridges public and private sectors. These collaborations are essential for building the infrastructure required for humanity’s next leap: establishing a permanent foothold on another world.
NASA has announced the date of the world’s first medical evacuation from the ISS. The Dragon spacecraft with the Crew-11 mission team will undock from the station on January 14.
Crew-11 mission members. Source: NASA
The medical issue aboard the ISS became known on January 7, when NASA canceled a spacewalk scheduled for the following day. Astronauts Mike Fincke and Zena Cardman were supposed to participate in the spacewalk.
Shortly thereafter, the aerospace administration announced that it would bring the Crew-11 mission team home early in order to better diagnose and treat this medical issue. NASA did not disclose which astronaut had fallen ill or what the problem was, citing privacy concerns. According to unofficial reports, it is 58-year-old Mike Fincke. This is his fourth flight into space and his third long-term assignment to the ISS.
At a subsequent press conference, NASA Chief Medical Officer James Polk declined to name the astronaut or disclose his diagnosis. However, he provided the following general description of the situation:
“This is not an operational issue. This was not an injury that occurred in the pursuit of operations,” Polk said. “It’s mostly having a medical issue in the difficult areas of microgravity, and with the suite of hardware that we have at our avail to complete a diagnosis.”
According to NASA’s plan, Crew-11 will leave the ISS on the evening of January 14. The next day, the spacecraft will splash down in the Pacific Ocean, where it will be picked up by the Shannon ship. Overloads during re-entry into the atmosphere can create additional risks for the astronaut — but NASA has well-developed scenarios for this case and instructions for ground crews.
After the departure of Crew-11, for the first time in many years, the ISS crew will be reduced to just three people. NASA astronaut Christopher Williams and Roscosmos cosmonauts Sergei Kud-Sverchkov and Sergei Mikayev will remain on board the station.
The launch of the next manned spacecraft to the ISS (Crew-12 mission) is currently scheduled for February 15. However, NASA is considering the possibility of postponing the date if possible.
A group of Australian scientists have revealed how we may be able to learn to speak with aliens, and the answer is found right here on Earth.
If we do make contact with extraterrestrial life, it will likely require sending messages across vast distances of interstellar space.
The question for astronomers looking out for distant civilisations is how this communication would even be possible if we don't share a language.
Now, scientists say we might be able to develop a 'universal language' with an unlikely inspiration: The humble honeybee.
With six legs, five eyes, and a radically different social structure, scientists say that bees are among the closest things we have to aliens here on Earth.
Although humans and bees have wildly different brains, we have both evolved complex methods of communication and cooperation.
More importantly, new research shows that bees also have another very important thing in common with humans, which is the ability to do maths.
Scientists say we might learn how to communicate with aliens by studying the concepts that we share with honey bees
One of the big problems for communicating with aliens is the enormous distances involved.
Given that the nearest star to the sun is 4.4 light-years away, it would take an absolute minimum of 10 years to send a message and get a reply.
This makes it impractical to try to learn an alien's language from scratch, like in the sci-fi movie Arrival.
Instead, scientists want to develop a universal language that can be understood by any species, regardless of how they communicate.
To find a solution to this puzzle, the researchers asked how we might communicate with one of the most alien-like species on Earth.
Co-author Dr Adrian Dyer, of Monash University, told the Daily Mail: 'Because bees and humans are separated by about 600 million years in evolutionary time, we developed very different physiology, brain size, culture.'
However, despite these enormous differences, both humans and bees seem to have a similar basic understanding of mathematics.
Scientists have found that bees can learn to add and subtract in specialised tests, giving credence to the idea that mathematics might be a universal language
The researchers set up experiments in which bees could participate in maths tests to receive a reward of sugar water.
Incredibly, bees even demonstrated an ability to link abstract symbols with numbers, in a very simple version of how humans learn the Arabic numerals.
The fact that such a different organism shares mathematical concepts with humans lends evidence to the theory that mathematics could be a universal language.
The idea that mathematics could be the basis of alien communication is not a new theory.
In fact, the covers of the Golden Records, which accompanied the Voyager 1 and Voyager 2 space probes launched into deep space in 1977, were carved with mathematical and physical quantities.
Likewise, when researchers broadcast the Arecibo radio message into space in 1974, it contained 1,679 zeros and ones, ordered to communicate the numbers 1 to ten and the atomic numbers of the elements that make up DNA.
However, scientists weren't sure whether aliens would have similar enough mathematical concepts to understand these messages.
If bees can understand maths, then aliens might share those same universal concepts. That means attempts to communicate with mathematics, such as the cover of the golden disks on Voyager One and Two, could be successful
In their new paper, the researchers argue that their evidence from bees suggests that maths really is universal.
Dr Dyer says: 'When we tested bees on mathematical type problems, and they could build an understanding to solve the questions we posed, it was very interesting, and convincing that an alien species could share similar capabilities.'
'Now we know maths can be solved by bees, we have a solid basis to think about how to try to communicate with alien intelligence.'
As to what that language might look like, Dr Dyer says it may be very similar to the mathematics most of us use every day.
'Mathematics, which was first developed by philosophers to communicate complex problems more efficiently, is already a language we humans use every day.
'At a simple level, binary coded information would be a start, then, like we humans learn language through many "baby steps", we learn with another species to build a commonly understood language framework.'
The Drake Equation is a seven-variable way of finding the chance of active civilizations existing beyond Earth.
It takes into account factors like the rate of star formation, the amount of stars that could form planetary systems, the number potentially habitable planets in those systems.
The equation includes recent data from Nasa's Kepler satellite on the number of exoplanets that could harbor life.
Researchers also adapted the equation from being about the number of civilizations that exist now, to being about the probability of civilization being the only one that has ever existed.
Researchers found the odds of an advanced civilization developing need to be less than one in 10 billion trillion for humans to be the only intelligent life in the universe.
Unless the odds of advanced life evolving on a habitable planet are astonishingly low, then humankind is not the only advanced civilization to have lived.
But Kepler data places those odds much higher, which means technologically advanced aliens are likely to have existed at some point.
A 10-second signal from one of the most distant points in the universe has been detected by humanity, and scientists are still trying to understand its origins.
Two Earth satellites have confirmed that the mysterious signal came from a point 13billion light-years away from Earth, likely coming from an exploding supernova when the universe was only 730million years old.
The farther away something is in space, the longer its light (or signal) takes to reach us, so when humans see a very distant explosion or star, we're actually looking at what happened there billions of years ago, like a time machine showing us the past.
In this case, scientists believe this high-energy gamma-ray burst, which they've named GRB 250314A, came from the earliest supernova ever recorded from the dawn of time.
Gamma rays are invisible and ultra-powerful forms of light. They are the most energetic source of radiation known in the universe, which is produced by massive stellar explosions, appearing as super-bright flashes from our planet.
Scientists are still unsure why this ancient supernova from the early universe looks almost exactly like the exploding stars seen in our nearby modern universe today.
If this explosion is the true source of the signal, researchers from NASA and the European Space Agency (ESA) expect early stars to be bigger, hotter, and produce much more volatile explosions than the mysterious signal suggested.
Andrew Levan, lead author of a new study on the signal from Radboud University in the Netherlands, said: 'There are only a handful of gamma-ray bursts in the last 50 years that have been detected in the first billion years of the universe. This particular event is very rare and very exciting.'
A gamma-ray burst named GRB 250314A (Pictured) is believed to the be the source of a mysterious signal received from 13billion light-years away
An artist's impression of the supernova GRB 250314A as it was exploding during the first billion years after the Big Bang
The signal was first discovered on March 14, 2025, when the Space Variable Objects Monitor (SVOM) satellite picked it up as a sudden flash of high-energy light from deep space.
However, two studies on the possible source of this distant signal have just been released.
The probe is a joint project between scientists in France and China designed to spot these kinds of bursts throughout the cosmos.
The signal scientists recorded was a short, powerful burst of gamma rays, which are invisible waves of energy stronger than X-rays and capable of passing straight through the human body, damaging cells, DNA, and tissues.
Since this burst likely came from an exploding star 13billion light-years from Earth, however, the gamma rays that reached Earth were far too weak to pose any danger to people.
This burst lasted only about 10 seconds because gamma-ray bursts are like quick fireworks in space, releasing a huge amount of energy in a very short time before fading away.
Unlike random noise or background static in space, which is constant and weak, these gamma-ray bursts stand out as super-bright, focused beams with a unique pattern that human satellites have been built to recognize.
NASA's James Webb Space Telescope (JWST) confirmed the discovery about three and a half months later, during the summer of 2025, by taking detailed pictures and measurements of the fading glow of the explosion, which could still be seen in space.
The 10-second signal was recorded in 2025 by the Space Variable Objects Monitor (SVOM) satellite, operated by France and China
'Only Webb could directly show that this light is from a supernova — a collapsing massive star,' Professor Levan added in a statement from NASA.
Other sources of mysterious space noise like this might include solar flares or cosmic rays, but gamma-ray bursts are much rarer and come from massive events like star explosions that scientists are able to track down billions of years after they take place.
Levan added that JWST is so advanced that scientists believe it'll be able to find more signals from when the universe was only five percent of its current age, which is roughly 14billion years old now.
To this point, scientists know very little about the first billion years of the universe, what was happening in space during this time, or how stars behaved and died throughout the cosmos.
Until now, it was thought that following the Big Bang, the massive explosion believed to have kickstarted everything in existence, early stars lived much shorter lives and contained fewer elements than stars like our sun do today.
However, in December 2025, the new studies published in the journal Astronomy & Astrophysics analyzed detailed observations from the Webb Telescope and found that this supernova from 730 million years after the Big Bang had the same brightness and radiation signature as exploding stars billions of years later.
Nial Tanvir, a professor at the University of Leicester in the UK, added: 'Webb showed that this supernova looks exactly like modern supernovae.'
Astronomers witnessed a cosmic explosion that released energy equivalent to 400 billion suns. It was caused by a supermassive star being torn apart by ablack hole.
Absorption of a star by a supermassive black hole (concept). Source: Caltech/R. Hurt (IPAC)
The event, officially designated AT2024wpp (and informally named Whippet), was first discovered by astronomers as part of the Zwicky Transient Facility sky survey. It immediately attracted attention due to its similarity to the cosmic explosion AT 2018cow, which was 10–100 times brighter than an average supernova.
Whippet also resembled another class of objects called “Luminous Fast Blue Optical Transient” (LFBOT). This is an incredibly bright burst of light visible at distances of up to billions of light-years, which usually lasts for several days and emits high-energy radiation ranging from the blue end of the spectrum to ultraviolet and X-rays. Although several dozen such phenomena have been detected, LFBOTs remain poorly understood, although scientists associate them with the destruction of stars.
To solve the mystery of Whippet, researchers observed it using the Liverpool Telescope in the Canary Islands and the Swift spacecraft. They confirmed that its spectrum was shifted toward the blue end of the spectrum and that the object emitted X-rays, as expected from an LFBOT. This, combined with the fact that Whippet had an extremely high temperature, led to the conclusion that the event was caused by a black hole tearing apart a star with its gravity.
Further investigation by Whippet revealed a powerful shock wave propagating from the central source at about 20% of the speed of light, colliding with the surrounding gas. These shock waves dissipated in about six months when they reached the outer gas bubble left over from the destroyed star.
However, scientists have not yet fully understood all the circumstances surrounding Whippet. The team discovered helium moving away from the source at a speed of about 21 million km/h. This suggests that some densely bound structure survived tidal disruption and is moving at a speed of about 2% of the speed of light.
The team believes that this could be a stream of material ejected by the core of a doomed star when it was “spaghettified” by the black hole at the center of Whippet. Another possibility is that this stream of helium was generated by a third body in the system when it was exposed to particles and X-rays ejected by the black hole that had just “devoured” the star.
NASA’s Curiosity rover, which has been exploring the Red Planet for more than 13 years, has sent back a stunning new panorama. Taken from the summit of Mount Sharp, the image reveals a stark but breathtaking view of the landscape bathed in the rays of the setting sun.
NASA’s Curiosity rover photographed this panorama from the slopes of Mount Sharp inside Gale Crater, combining images taken on two different Martian days in November 2025 to highlight the change in light. Photo: NASA/JPL-Caltech
Observation point
In November 2025, the rover’s navigation cameras captured black-and-white images over two Martian days (sols). Specialists combined them into a single composite panorama, using blue and yellow tones to highlight changes in lighting. This technique helps to better see the details of the terrain.
Curiosity took this image from the top of a ridge overlooking a unique area known as the Boxwork. This is a maze of mineral ridges created billions of years ago by underground waters flowing through cracks in the rock. Softer rocks eroded over time, leaving behind hard “veins.” Such structures are key evidence of Mars’ wet past.
Image taken by the Curiosity rover on July 25, 2025. Source: NASA/JPL-Caltech/MSSS
The rover recently drilled into this ridge to collect a rock sample for analysis. In the foreground of the panorama, you can see tracks from its wheels and traces of previous drilling. Curiosity’s goal is to study how the planet evolved from a wet environment, potentially suitable for microbial life, to a dry desert.
Maximum efficiency
Despite its age, the Mars rover has gained new autonomous capabilities thanks to software updates. This allows it to plan its research more effectively and collaborate with orbital spacecraft, optimizing the performance of its aging energy system.
The panorama from Mount Sharp is not only an impressive sight, but also a reminder of the persistent work of the research robot. Each new sample and photograph brings science closer to solving the main mystery: whether there was ever life on Mars.
Deep-sea trenches are deep depressions at the bottom of the Earth’s oceans, which are unique features of our planet in the Solar System. They were formed as a result of the movement of tectonic plates and can reach depths of 10-11 km, creating one of the most amazing landscapes on our planet – the hadal zone.
What do you know about deep-sea trenches? Source: geographical.co.uk
Space at the bottom
There are places on our planet whose gloomy mystery can rival the darkness of space itself. Usually, these include Antarctic glaciers, where life is almost impossible, or the polar deserts on some islands of the Canadian Arctic Archipelago, which are often compared to Mars.
However, there are places on Earth that are almost as inaccessible to humans as outer space, even though they are as far away from it as possible. These are deep-sea trenches – narrow and long depressions at the bottom of the world’s oceans, whose bottoms are never reached by sunlight. Their landscape resembles that of a celestial body, and their few inhabitants resemble aliens.
However, to truly understand the depth of the trenches, you need to observe what happens when you gradually walk along the seabed, going deeper and deeper.
Littoral zone. Source: Wikipedia
First, they determine the area between the highest point that gets underwater during high tide and the one that remains dry during low tide. This is called the littoral zone, and it is usually a narrow strip along the coast that sometimes gets a few kilometers wide. A great example of a littoral zone is a bunch of Ukrainian estuaries: looking at them, it is clear that the littoral zone is an area that makes any other part of the seabed seem deep.
Next comes the continental shelf – a section of the seabed where the depth slowly decreases to 200 m. The northern part of the Black Sea or the English Channel area, where the depth may not exceed hundreds of meters, tens of kilometers from the coast, are typical example. In essence, the shelf is part of the continental mass submerged by the ocean. Between the sedimentary rocks and basalt, as in much drier places, there is a layer of granite.
If you continue further, you will reach the continental slope, where the bottom descends at a much greater angle and quickly reaches a depth of 2-3 km. The continental slopes are particularly pronounced. For example, off the coast of North America.
The bottom of the World Ocean. Source: Wikipedia
Further down, the angle of the seabed decreases again, and abyssal plains stretch to depths of 4-5 km. These are huge depressions, comparable in size to entire countries, bounded by continental slopes. Sunlight rarely reaches their bottom, and despite the fact that bathyscaphes have repeatedly descended there, we still know less about these areas than we do about the surface of the Moon.
Deep-sea trenches are located even deeper than abyssal plains. The term “hadal zone” is used to describe the fauna of this landscape. There is no need to talk about flora, as it is practically non-existent at depths greater than 5 km. These are truly abysses, where the bottom slopes steeply downward and no light penetrates.
Formation of oceanic trenches
The fact that all the deepest areas of the ocean are shaped like narrow, elongated strips stretching along the coasts of continents or island arcs can be explained by the peculiarities of their formation. As is well known, the Earth’s crust consists of large blocks – tectonic plates. They move along the viscous, relatively plastic outer layer of our planet’s mantle, and it is this movement that causes earthquakes and volcanic eruptions.
Formation of an oceanic trench
The crust of plates can be continental, i.e., contain the aforementioned layer of granite, or oceanic, i.e., consist only of basalt and sedimentary rocks. Some plates consist of both types, while others consist only of oceanic crust.
In most cases, the transition from the continental slope to the ocean depths involves the same tectonic plate. However, sometimes two different lithospheric blocks are encountered here: one with a continental crust and the other with an oceanic crust. In this case, the oceanic plate begins to subduct beneath the continental plate and partially melts. As a result, a deep depression is formed.
Its slopes are always gentler on the side of the subducting oceanic plate and steeper on the continental side. This is the structure we call a deep-sea oceanic trench. At the same time, the plate subducts very slowly, so from the outside it may seem like a completely calm place.
Pacific Ring of Fire. Source: Wikipedia
The way deep-sea trenches are formed determines their extremely uneven distribution across the surface of our planet. They are always located in tectonically active zones, mainly in the so-called Pacific Ring of Fire, which surrounds the largest ocean on our planet.
Mariana Trench
In fact, all ten of the deepest ocean trenches are located in the Pacific Ocean. There are more than thirty of them in total. For comparison, there are only three large trenches in the Indian and Atlantic Oceans, and none at all in the Arctic Ocean.
However, the most famous of the Pacific trenches is the Mariana Trench, which is also considered the deepest in the world. Its depth is estimated differently, but usually the value of 11,022 m is given. It is located in the western part of the Pacific Ocean, near the islands of the same name. Its bottom is so inaccessible that humans first reached it only in 1960, just a year before they first set foot on the surface of the Moon. Until recently, the number of people who had visited the bottom of this trench was smaller than the number who had visited our natural satellite.
Mariana Trench. Source: Wikipedia
The water pressure at this depth is 108.6 MPa, which is 1,072 times greater than normal atmospheric pressure at sea level. However, microorganisms, crustaceans, and even fish have been found there. None of them is found anywhere else except this place, and they have never seen the light of the sun or stars. Their living conditions resemble those in space.
In addition, despite its inaccessibility, the Mariana Trench already bears the negative traces of human activity. Heavy toxic waste settles there and, together with river water, flows into the oceans.
Other trenches
Everyone knows about the Mariana Trench. However, the rest are no less amazing than it. Tonga, Philippine, Kermadec, Izu Ogasawara, Kuril-Kamchatka, North New Hebridean, Bougainville, and Japan – all of them are deep enough to completely submerge Mount Everest.
The landscape of the Puerto Rico Trench. Source: www.wired.com
Although the Mariana Trench is the deepest, the title of the longest on Earth belongs to another Pacific structure – the Peru-Chile Trench. It stretches along the coast of South America for 5,900 km, where the Nazca Plate dives under the South American Plate.
The deepest and largest trench in the Indian Ocean is the Sunda Trench, which stretches for 4-5 thousand km along the coast of Indonesia. Its maximum depth is 7,729 m near the island of Bali.
The ocean trenches of the Atlantic Ocean are generally relatively short in length, as they are formed by small tectonic plates. The deepest of these is the Puerto Rico Trench, with a maximum depth of 8,742 m. This is only slightly less than the height of Mount Everest.
It would seem that ocean trenches have nothing to do with astronomy. However, when considering the planets of the Solar System, among the unique phenomena available only on Earth, along with the biosphere, it is worth mentioning them. After all, nowhere else do lithospheric plates move, and even more so, there are no places where they collide under a layer of liquid.
Artist's depiction of an ancient extant lake in Gale Crater. Credit - NASA/JPL-Caltech/MSSS
Mars has a curious past. Rovers have shown unequivocal evidence that liquid water existed on its surface, for probably at least 100 years. But climate models haven’t come up with how exactly that happened with what we currently understand about what the Martian climate was like back then. A new paper, published in the journal AGU Advances by Eleanor Moreland, a graduate student at Rice University, and her co-authors, has a potential explanation for what might have happened - liquid lakes on the Red Planet would have hid under small, seasonal ice sheets similar to the way they do in Antarctica on Earth.
To understand why this finding is significant, it's best to understand the “Faint Young Sun Paradox” in Mars research. According to data collected by the Curiosity Rover in Gale Crater, there was absolutely liquid water pooled on the surface of Mars at some point in its history. There were clear signs of deltas and even river channels carved into the rock, and the best estimates for when this hydrological cycle was active was around 3.5 billion years ago.
However, 3.6 billion years ago, the Sun was 25% dimmer than it is currently - and we already know Mars is frozen even at the Sun’s current output power. So how could liquid water, which must, by definition, exist in environments above freezing, endure on the surface of Mars while it was possibly even colder than it is today.
Water discusses the possibility of water on Mars
There have been two main solutions to this paradox put forward in the literature. One is that there were “bursts” of warming on Mars that were caused by either active volcanoes or asteroid impacts, that allowed liquid water to run freely, but only until the energy from those events dissipated. The other is that Mars was always cold and icy, but that the liquid water existed under permanent ice sheets.
To settle this debate, Ms. Moreland and her co-authors developed a new computer model called the Lake Modeling on Mars for Atmospheric Reconstructions and Simulations (LakeM2ARS). This software package takes inputs like a potential lake’s location, its size, and the atmospheric composition, and predicts how long it could have held onto its liquid water. The results of the model were rather counterintuitive.
In warm scenarios, where the ambient temperature was above freezing for a significant amount of time, evaporation actually made the lakes dry out quickly. Whereas, in cold scenarios, the lake would have developed seasonal ice cover, which would have acted as a barrier to the evaporation. It would have still allowed liquid water to actively exist on the surface during seasonal warm periods though. “Warm” is relative though, with only a small part of the year existing at an average of above 0 ℃. Most of the rest of the year the average temperature would have been closer to -20 to -30 ℃.
We still haven't found existing liquid water on Mars - as Fraser explains.
So how can researchers rule out permanent ice rather than the seasonal variety? If the atmosphere was too thin, that likely would have been the condition on Mars for millions of years. But, it also would have left distinct physical marks, such as dropstones and frost wedges, that weren’t present when Curiosity looked in Gale Crater. Seasonal ice provides a nice middle ground between the two extremes. It stopped the quick evaporation of the “warm and wet” climate model, while also explaining the absence of the features expected if the water was constantly frozen.
This study fits neatly into the ongoing discussion about the early climate on Mars, and what implications it might have had for the existence of life at some point on the planet. Luckily, we have another rover (Perseverance) wandering around different Martian terrain (Jezero Crater) that the LakeM2ARS software can be adapted to model that area, as well as other previously wet areas on Mars. As we continue our exploration of what is now a dry, arid world, the history of water will remain one of its most intriguing mysteries, even as we develop ever more sophisticated computer models to figure it out.
This illustration shows NASA's Perseverance rover with sample tubes on the Martian surface. Funding has been cut for the mission, effectively ending it. Image Credit: NASA/JPL-Caltech
It looks like NASA's Mars Sample Return (MSR) mission has come to a bureaucratic end. The mission was to be the crowning achievement in the study of Mars and all the questions surrounding its ancient habitability. But the US Congress has drastically cut the mission's funding.
Despite decades of study and technological improvement and innovation, the issue of Martian habitability has been difficult to solve. MSL Curiosity and Perseverance have widened and deepened our understanding of the planet, and have provided tantalizing evidence for warm, wet periods on Mars conducive to life. But the next step was to return Martian rock samples to Earth, where the investigative power of modern labs could be brought to bear on them.
As far back as 2011, returning samples from Mars was recognized as a high priority in NASA's planetary science endeavours. Even today, NASA's webpage for MSR states that "Mars Sample Return (MSR) would be NASA's and ESA’s (European Space Agency) ambitious, multi-mission campaign to bring carefully selected samples to Earth. MSR would fulfill one of the highest priority solar system exploration goals from the science community. Returned samples would revolutionize our understanding of Mars, our solar system and prepare for human explorers to the Red Planet."
The Perseverance rover was the first stage of the mission, and it has performed exceptionally well. The rover has gathered and cached 33 sample tubes of interesting rocks and dust, ready for retrieval by the MSR. Now, the fate of those samples is unclear.
NASA knew that they were in tough territory. The estimated cost to retrieve the samples ballooned to 11 billion dollars. After working on new mission architectures, they were able to get the estimated cost down to about 7 billion dollars. But those were just estimates, and because it's such an unprecedented mission, there was a clear lack of certainty around those numbers.
The issue is money. There's heavy pressure on NASA to reduce its budget, and although Congress refused to reduce it as severely as the President wanted, something had to give. Since the MSR still required large amounts of money, and since the technology to achieve it still wasn't clear, it was the obvious choice for cancellation. It became a high-profile political football, not just a science mission.
The mission was extremely complex. The current design involved sending a lander to the surface. Perseverance would deliver the sample tubes to the lander, and if that were not possible, a pair of small sample return helicopters would do the job. The lander also had a rocket which would carry the samples to Martian orbit. From there, it would rendezvous with an orbiting spacecraft that would send the samples back to Earth. To say this was a complex undertaking is an understatement.
*This artwork from 2022 shows the conceived mission architecture.
Image Credit: By NASA/ESA/JPL-Caltech
- https://photojournal.jpl.nasa.gov/catalog/PIA25326 (image link), Public Domain, https://commons.wikimedia.org/w/index.php?curid=121171927*
But isn't NASA all about American ingenuity and the spirit of exploration and adventure? You can't lead in science without money, and it's hard to argue that President Trump's request to inflate the USA's military budget to an unprecedented degree didn't have something do with NASA's budget cuts. He asked for 1.5 trillion dollars of military spending, a profligate 50% increase.
The budget still provides some money for developing technology related to further exploration of Mars, but only a small amount.
"As proposed in the budget, the agreement does not support the existing Mars Sample Return (MSR) program. However, the technological capabilities being developed in the MSR program are not only critical to the success of future science missions but also to human exploration of the Moon and Mars."
It continues: "Therefore. the agreement provides the request of $110,000,000 for the Mars Future Missions program, including existing MSR efforts, to support radar, spectroscopy, entry, descent, and landing systems, and translational precursor technologies that will enable science missions for the next decade, including lunar and Mars missions."
*Perseverance's cached samples await retrieval on the Martian surface.
Image Credit: NASA/JPL-Caltech/MSSS*
It's possible that some of that money will lead to new technologies, and a more budget-friendly way of retrieving the cached samples. But that is far from certain. It's also possible that technology will be developed that can study the samples effectively on the surface and returning them to Earth won't be necessary. But the technology in Earthly labs will advance at the same rate. It's difficult to conceive how studying them on Mars will ever be as effective as studying them on Earth.
Politics can't be ignored in this issue. NASA was teaming up with the ESA on this mission. But with the current administration's threats against European countries and the EU, which include using military force to sieze Greenland—otherwise known as war—that cooperation is likely dead. Maybe never to be revived.
The future is always unwritten and unknown. Maybe the MSR will be revived at some point in the future. Maybe the ESA will go it alone. China has plans for a Mars sample return mission, and now the path is clear for them to be the first to return Martian samples to Earth. However, their mission is not as sophisticated as the NASA/ESA mission. While Perseverance's samples are carefully chosen for maximum science benefit, China's mission is more of a grab and go endeavour.
Fortunately, the sample tubes are likely to sit there waiting for a long time, unlikely to be degraded in Mars' cold, dry environment. But for scientists who have put their hearts and minds into this ambitious mission, the news must be crushing.
Chandra image of Kepler's Supernova, with colors representing the different levels of X-ray energy in the expelled debris. Credit: NASA
In 1604, German astronomer Johannes Kepler spotted a new star in the sky that was so bright it could be seen during the daytime. The discovery, which Kepler described in his book *De Stella Nova*, caused quite a stir in the astronomical community. With this one point of light, astronomers questioned the prevailing dogma that the "firmament" (the background stars in the sky) was not unchanging and permanent. In time, we would come to realize that Kepler's Supernova (as it's come to be known) was a white dwarf that exceeded its critical mass and exploded in a brilliant burst.
Located about 17,000 light-years from Earth in the constellation Ophiuchus, Kepler's Supernova is a prime example of a Type 1a supernova. These occur when a white dwarf in a binary system pulls material from its companion star or merges with another white dwarf. Its proximity to Earth has allowed the Chandra X-ray Observatory to capture detailed images of the supernova remnant, which astronomers have used to monitor its evolution over time. Based on data acquired between 2000 and 2025, the science team has created the longest-spanning video of the debris field left by this supernova.
Supernova remnants, which consist of massive clouds of dust and gas expelled from the star, are heated to millions of degrees by the heat of the explosion. This causes the material to glow brightly in different wavelengths (often in X-ray light), which Chandra has monitored using its advanced X-ray optics. Combined with the longevity of the mission, which has been in operation for a quarter of a century, Chandra has monitored changes in the remnant cloud very closely.
Jessye Gassel, a graduate student at George Mason University in Virginia, led the work on this video. It and the associated research were presented by Gassel at the 247th meeting of the American Astronomical Society in Phoenix. "The plot of Kepler’s story is just now beginning to unfold," he said in a Chandra press release. "It’s remarkable that we can watch as these remains from this shattered star crash into material already thrown out into space."
A particularly interesting part of this video is how it shows different parts of the remnant moving at incredible speeds in different directions. While the fastest parts are traveling at about 2% the speed of light (22.2 billion km/h; 13.8 billion mi/h) downwards, the slowest parts are traveling at 0.5% the speed of light (6.4 billion km/h; 4 billion mi/h) upwards. This difference is due to the gas the remnant is pushing toward the top of the image being denser than the gas it is pushing toward the bottom. This provides scientists with information about the supernova's environment.
Another interesting feature is the widths of the rims forming the blast wave of the supernova, the leading edge of the explosion that encounters material outside the star first. By examining how wide and fast it was, the team gained vital information about the star's explosion and its immediate surroundings before they were disturbed. "Supernova explosions and the elements they hurl into space are the lifeblood of new stars and planets," said Brian Williams, the principal investigator of the new Chandra observations. "Understanding exactly how they behave is crucial to knowing our cosmic history."
According to the new compromise spending bill for the current fiscal year, it appears Congress has given in to the White House’s demands that resources needed to complete the planned Mars Sample Return (MSR) program be explicitly excluded from any approved budget. While the bill still awaits a final vote in Congress and the President’s signature, NASA officials are sending signals that the MSR program is effectively dead.
“The agreement does not support the existing Mars Sample Return program,” the bill states.
Victoria Hamilton, a planetary scientist at the Southwest Research Institute (SwRI) and chair of NASA’s Mars Exploration Program Analysis Group, described the death of MSR as “deeply disappointing” while also questioning the veracity of the current administration’s stated goals.
“When we’ve got memos coming out saying we want to be the dominant power in space, I wonder how we leave something this ambitious behind,” Hamilton said.
Escalating Cost of Retrieving Martian Rocks has Haunted the MSR Program
Before NASA launched Perseverance in July 2020, mission planners had struggled with the concept of retrieving the samples the rover was tasked with collecting through its mission. Since then, the interplanetary explorer has collected dozens of samples and stored them for the planned future return.
Artist’s concept of the Mars ascent rocket, one component of the effort to collect and send samples of Martian rock back to Earth
(NASA/Public Domain).
During that time, the cost for MSR has continued to rise, with 2024 estimates reaching $11 billion. Regardless of the potential scientific value, the extraordinarily large share of NASA’s science budget that the single mission was projected to consume left planetary scientists working on other stalled or underfunded projects wondering whether the MSR was worth the broader scientific cost.
Repeated threats from Congress to scrap the ambitious yet costly program altogether resulted in a new, stripped-down plan released in January 2025 that came closer to the original $7 billion estimate. Now, it appears even that plan was still too rich for the current administration’s taste, resulting in its explicit exclusion from the new bill.
Funding Could Aid Other Missions and Keep Hopes of MSR Alive
As advocates of the MSR program try to regroup and seek other alternatives to bring the Martian rocks back to Earth to study, NASA’s proposed $7.25 billion science budget offers some hope that a future mission may not be completely off the table.
For example, the bill, which cuts roughly 1% from the 2025 budget, allocates $110 million for a “Mars Future Missions” program to continue developing the key technologies needed for any future sample-return mission. These include further development of landing systems that can survive the thin atmosphere during descent, which has proven challenging and costly for previous missions.
Europa Lander prototype.(Credit: NASA/JPL-Caltech)
Assuming the bill is signed into law, other missions that have waited patiently for MSR to run its course may see new signs of life. For example, recent discoveries on the moons of Jupiter and Saturn and in the atmosphere of Venus have led to plans for missions to further explore those tantalizing findings. These include plans to explore potential subsurface oceans on Enceladus and Europa for extraterrestrial life.
Is the Search for Extraterrestrial Life on Mars Dead?
Although the newly proposed NASA science budget adds hope to the search for life on other moons and planets, proponents of MSR note the tantalizing cache of samples already collected by the rover since its 2021 arrival.
In 2024, mission operators spotted a surface feature containing mineral deposits called “leopard spots” in a dry riverbed that leads to Jezero crater. NASA scientists note that on Earth, these types of leopard spots are often left by microbial organisms interacting with the rock, making the Chevaya Falls sample arguably the best candidate for containing signs of past life on Mars.
Bethany Ehlmann, a planetary scientist at the University of Colorado Boulder, said scientists eagerly await the opportunity to examine these samples in Earth labs equipped to determine if they do hold signs of extraterrestrial life. Elhman also pointed to the potential for other scientific discoveries that the dozens of samples gathered by Perseverance may hold.
“A rock with a potential biosignature is awaiting return now, and other rocks hold breakthrough discoveries,” the UC Boulder scientist explained.
Unless Congress has an unexpected last-minute change of heart, the new budget has left mission planners wondering about the fate of the samples, as the rover has nearly finished filling its collection tubes.
“We’d really like to hear from NASA sooner than later that they will work with the community on a plan to get these samples,” Hamilton said.
Christopher Plain is a Science Fiction and Fantasy novelist and Head Science Writer at The Debrief. Follow and connect with him on X, learn about his books at plainfiction.com, or email him directly at christopher@thedebrief.org.
NASA’s Hubble Space Telescope has spotted an astronomical object unlike any previously observed, revealing an unusual remnant of the cosmic past.
The object, which astronomers say is a dark matter cloud void of any stars, but billowing with cosmic gases, has been dubbed “Cloud-9” and represents the first confirmed detection of such an unusual object.
The object’s unique appearance offers astronomers a unique look at the evolution of galaxies early in their formation process and could provide new insights into the mysterious nature of nonluminous dark matter.
“A Tale of a Failed Galaxy”
The absence of stars within Cloud-9 served as a key observation, according to principal investigator Alejandro Benitez-Llambay of the Milano-Bicocca University in Milan, Italy.
“In science, we usually learn more from the failures than from the successes,” Benitez-Llambay said in a statement. “In this case, seeing no stars is what proves the theory right.”
Characterizing Cloud-9 as the cosmic remnant that conveys “a tale of a failed galaxy,” Benitez-Llambay said the discovery offers astronomers a rare glimpse of “a primordial building block of a galaxy that hasn’t formed.”
Above: An annotated “compass” view of Cloud-9, which astronomers categorize as a Reionization-Limited H I Cloud (RELHIC), as captured by the Hubble Space Telescope’s ACS (Advanced Camera for Surveys) and the ground-based Very Large Array (VLA) radio telescope (Image Credit: Science: NASA, ESA, VLA, Gagandeep Anand (STScI), Alejandro Benitez-Llambay (University of Milano-Bicocca); Image Processing: Joseph DePasquale (STScI)).
A Cosmic “RELHIC”
Cloud-9 represents a new class of objects known as Reionization-Limited H I Clouds (RELHICs), where “H I” represents neutral hydrogen. Combined, the term was devised by astronomers to convey the presence of a hydrogen cloud that formed early in the universe, and which had not yet produced any stars.
Like cosmic phantoms, these kinds of objects were long hypothesized, but had never been directly observed until now. Before the recent Hubble observations, astronomers may have mistaken Cloud-9 for a faint dwarf galaxy invisible to telescopes on Earth, as they lack the sensitivity required to detect any stars that might have been lurking in its gaseous body.
“With Hubble’s Advanced Camera for Surveys, we’re able to nail down that there’s nothing there,” said Gagandeep Anand of STScI, the lead author of a new study detailing the discovery.
A Window to the Dark Side
“We know from theory that most of the mass in the universe is expected to be dark matter, but it’s difficult to detect this dark material because it doesn’t emit light,” according to Andrew Fox, a member of the discovery team with the European Space Agency’s Association of Universities for Research in Astronomy/Space Telescope Science Institute (AURA/STScI).
Comparing the cosmic relic to “a window into the dark universe,” Fox said that Cloud-9 has offered he and his international colleagues behind the discovery “a rare look at a dark-matter-dominated cloud.”
A New Theory Emerges
According to current theories, RELHICs may represent clouds composed of dark matter that have failed to accumulate the amount of gas required to form stars. Based on its presence alone, astronomers now hypothesize that Cloud-9 may be the first detection of a variety of small, dark matter-rich failed galaxies that are likely found throughout the universe.
These unique structures have likely evaded detection in the past because traditional observation methods make them very difficult to spot, as they are void of bright objects like stars.
Another unique feature about Cloud-9 is that the clouds it possesses are smaller and more uniform when compared to hydrogen cloud formations observed closer to the Milky Way. Cloud-9 is also closer to possessing a perfect spherical shape, which also contributes to its unique appearance.
With a neutral hydrogen core approximately 4,900 light-years in diameter, based on radio signals emanating from the object. This leads astronomers to conclude that Cloud-9 has a mass roughly one million times greater than that of our Sun. If this estimate is correct, that would mean that the dark matter the object possesses would be equivalent to five billion solar masses.
Failed galaxies like Cloud-9 are unique, as they represent structures that are quite unlike most astronomers observe in our universe. Their study lends themselves to the study of dark matter, as well as the mysteries surrounding unusual region that are void of stars—a characteristic that makes them difficult to observe due to the presence of more luminous objects nearby.
Although Cloud-9’s discovery first occurred three years ago during the radio survey of the Five-hundred-meter Aperture Spherical Telescope (FAST) in Guizhou, China, the discovery was later confirmed by observations made by the Green Bank Telescope and the Very Large Array facilities in the United States.
Still, Hubble’s keen eye, made possible from its position in space, was required to conclusively rule out the presence of any stars that would have been too faint for even the most powerful telescops on Earth to detect.
Cloud-9’s confirmation marks an astronomical first, and although such objects had been hypothesized to exist, the discovery was still surprising, according to team member Rachael Beaton of STScI, who compared the unique celestial object to an empty cosmic home, of sorts.
“Among our galactic neighbors, there might be a few abandoned houses out there,” Beaton said.
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 atmicah@thedebrief.org. Follow him on X @MicahHanks, and at micahhanks.com.
NASA releases rare close-up images of interstellar comet 3I/ATLAS
NASA releases rare close-up images of interstellar comet 3I/ATLAS
Story by Modern Engineering Marvels
A staggering 250,000 kilometers per hour was the speed at which the comet had rushed through the inner solar system near the Sun–a reminder of how extreme velocities set interstellar visitors apart from homegrown comets. That velocity set the stage for NASA’s newly released close‑up views of 3I/ATLAS, captured by three spacecraft at Mars as the object swept just 18 million miles from the planet, a very unusually intimate pass for an object born around another star.
Image Credit to Wikimedia Commons | License details
The sharpest imaging came from the HiRISE camera aboard the Mars Reconnaissance Orbiter, which resolved a compact coma appearing as a bright, pixelated sphere at about 19 miles per pixel. While modest in appearance, these data provided crucial constraints on both nucleus size and dust environment. MAVEN’s ultraviolet instrument added a layer of chemical insight to the campaign, as its design for probing tenuous atmospheric gases lent itself to detecting hydrogen signatures tied to water breakdown, thus providing an upper limit on the comet’s deuterium‑to‑hydrogen ratio, an important tracer of the comet’s formation region. Composition-sensitive ultraviolet data of this sort are extremely rare for interstellar objects.
This multi‑spacecraft campaign corresponds to an unprecedented solar system–wide effort. Per ESA, twelve NASA assets have imaged 3I/ATLAS since July, including heliophysics missions that could observe the comet near the Sun when Earth-based telescopes couldn’t track it through the intense glare. Those vantage points allowed for continuous monitoring as 3I/ATLAS passed behind the Sun, enabling high‑cadence studies of its evolving tail geometry. Newly processed images from SOHO and NASA’s PUNCH mission showed the dust tail in late September and early October, capturing distinct jets that intensified after perihelion in late October.
3I/ATLAS as seen from Mars.
Photo shared by NASA Photograph: (NASA)
The pace of the observations then quickened when the James Webb Space Telescope joined the campaign. Its infrared spectrograph measured an unexpected chemical signature: the coma contains nearly eight times as much CO₂ as water vapor. This inversion of the typical cometary ratio is unlike almost every well‑studied solar system comet. “I have never seen such a strong CO2 peak in a comet spectrum,” said Martin Cordiner of NASA Goddard. Because Earth’s atmosphere blocks the relevant infrared wavelengths, only Webb could uncover this composition, hinting that 3I/ATLAS may preserve ice chemistry inherited from a star-forming environment very different from the Sun’s.
Such chemical fingerprints are complemented by orbital analyses that suggest great age. As NASA’s Tom Statler pointed out, the comet may have originated in a system older than the solar system itself: “gives me goose bumps to think about.” Its hyperbolic trajectory confirms that it is indeed an interstellar visitor, and integrations backward in time of its motion indicate it approached from the constellation Sagittarius with a heliocentric velocity in excess of 58 km/s. Investigations using the stellar data from the European Space Agency’s Gaia spacecraft demonstrate that the distribution of the velocity of the comet is indicative of objects that have been ejected from the Milky Way thin disk-a stellar population which contains long‑lived, moderately metal‑poor systems. These results support early theoretical predictions that 3I/ATLAS may have formed billions of years ago.
Amateur astronomers have seized the moment as the comet moves through the predawn sky. Observers say small telescopes can capture a faint, fuzzy glow-an accessible signpost of cosmic material that spent eons drifting between stars before its brief appearance near Earth. Indeed, as NASA’s acting astrophysics director Shawn Domagal‑Goldman put it, “Everyone that is in control of a telescope wants to look at it because it’s a fascinating and rare opportunity.”
Meanwhile, the scientific race goes on, as ESA’s Juice spacecraft conducts its own observations. The main antenna is now serving as a heat shield near the Sun, delaying data return until February, but its unusual geometry also means it will provide some of the highest‑quality post-perihelion measurements. When those data do arrive, they will be joining a rapidly growing archive of multi-wavelength studies and form the most complete portrait ever assembled of an interstellar comet during one solar system passage.
In its preliminary data release, taken from just seven nights of observations, the powerful Vera C. Rubin Observatory has discovered an enormous, fast-spinning asteroid that sets a new record.
An artist’s illustration of the massive, fast-spinning asteroid 2025 MN45, discovered in the first data from the Vera C. Rubin Observatory.
(Image credit: NSF–DOE Vera C. Rubin Observatory/NOIRLab/SLAC/AURA/P. Marenfeld)
Scientists analyzing the first images from the Vera C. Rubin Observatory have discovered the fastest-spinning asteroid in its size class yet.
The record-breaking space rock, called 2025 MN45, is larger than most skyscrapers on Earth at about 2,300 feet (710 meters) wide. The massive rock completes a rotation in about 113 seconds — making it the fastest-spinning known asteroid over 1,640 feet (500 meters) in diameter.
The research, published in The Astrophysical Journal Letters Wednesday (Jan. 7), is part of an asteroid survey aimed at improving our understanding of how these small bodies formed and evolved.
The study is the first peer-reviewed paper from the Rubin Observatory's LSST Camera — the largest digital camera in the world — which will repeatedly scan the Southern Hemisphere's night sky over 10 years to create an unprecedented time-lapse movie of the universe.
Rocks that roll
Asteroids are essentially large space rocks, and many are remnants of how our solar system appeared early in its 4.5 billion-year-old history, before the evolution of planets and moons. Therefore, by studying asteroids, scientists can figure out how our solar system changed over the eons.
Scientists found 2025 MN45 using the preliminary data release from the Rubin Observatory, which has already revealed thousands of previously unknown asteroids around the solar system after just seven nights of observations. (The 10-year LSST survey has yet to formally begin, but is expected to start in the next few months.)
The asteroid's remarkably fast spin excited the team, as it provides clues about the ancient rock’s composition.
"Clearly, this asteroid must be made of material that has very high strength in order to keep it in one piece," Sarah Greenstreet, an assistant astronomer at the National Science Foundation's National Optical-Infrared Astronomy Research Laboratory, said in a statement. "It would need a cohesive strength similar to that of solid rock."
"This is somewhat surprising," added Greenstreet, who also leads a Rubin working group about near-Earth objects and interstellar objects, "since most asteroids are believed to be what we call 'rubble pile' asteroids, which means they are made of many, many small pieces of rock and debris that coalesced under gravity during solar system formation or subsequent collisions."
This lightcurve shows how the asteroid’s brightness (x-axis) changes as it rotates (y-axis). Analyzing the curve allowed the team to calculate the asteroid's rotation speed, which sets a new record among asteroids of its size. (Image credit: NSF–DOE Vera C. Rubin Observatory/NOIRLab/SLAC/AURA/J. Pollard. Acknowledgement: PI: Sarah Greenstreet (NSF NOIRLab/Rubin Observatory))
Thousands more to come
In general, fast-spinning asteroids could have reached that state after a collision with another space rock, the study team said. It is also possible that 2025 MN45 is a remnant of a much larger asteroid that was shattered by a cosmic crash.
Most asteroids in the solar system are in the main asteroid belt between Mars and Jupiter. But most fast-spinning asteroids that astronomers have observed are much closer to Earth, simply because they are easier to see, the study authors noted. 2025 MN45 is a main-belt object, where most asteroids (as they are loose piles of rubble) must take at least 2.2 hours to rotate in order to avoid fragmentation. Anything that rotates faster than that "must be structurally strong," they wrote.
That said, 2025 MN45 is not the only fast spinner in the main asteroid belt. In addition to 2025 MN45, Rubin's first dataset includes 16 "super-fast" rotators, each of which has a rotational period of between 13 minutes and 2.2 hours, as well as two "ultra-fast" rotators with spins of less than two minutes each. All of these asteroids are also longer than 100 yards (90 m), and all but one of the newfound asteroids lives in the main belt.
The commissioning data from Rubin, which was released last June, underwent a deeper look in the new paper, which was also discussed Wednesday at a news conference at the 247th meeting of the American Astronomical Society in Phoenix.
The huge set of observations has about 1,900 never-before-seen asteroids, according to the statement. There will be many more to come when Rubin formally begins its 10-year survey of the sky in the coming months.
In particular, the initial results suggest that crashes may not be the only way asteroids reach extreme speeds, perhaps pressing astronomers to develop new explanations.
Europa, een van de vele manen van Jupiter, is een van de meest veelbelovende plekken om buitenaards leven te vinden in ons zonnestelsel. Onder een kilometers dikke ijslaag bevindt zich wellicht een oceaan van vloeibaar water. Maar uit een nieuwe studie blijkt dat de zeebodem mogelijk geologisch dood is en dat zet een flinke domper op de hoop dat Europa leven kan herbergen.
Op aarde wemelt het van het leven rond hydrothermale bronnen op de oceaanbodem. Dat zijn plekken waar scheuren in de aardkorst zeewater in contact brengen met vers gesteente. Bij die interactie komen allerlei chemische stoffen vrij die micro-organismen als energiebron kunnen gebruiken. Geen zonlicht nodig.
Wetenschappers koesteren al decennialang de hoop dat er zich onder de oppervlakte van Europa iets gelijkaardigs voordoet. De Jupitermaan heeft een oceaan die zo’n 97 kilometer diep is. Als er op de bodem breuken zouden ontstaan door tektonische activiteit, zou dat de perfecte omgeving kunnen zijn voor primitief leven.
Te weinig kracht om de bodem te breken
Maar daar zit nu het probleem. Amerikaanse onderzoekers hebben berekend hoeveel spanning er nodig is om breuken te laten bewegen op Europa’s zeebodem. Daarna keken ze naar alle bekende krachten die zulke spanning zouden kunnen veroorzaken.
De resultaten zijn ontmoedigend. De getijdenkracht van Jupiter, die Europa elke 84 uur een beetje uitrekt en samenperst, levert slechts ongeveer 3 procent van de benodigde spanning op. Zelfs als je aanneemt dat het gesteente al verzwakt is door miljarden jaren aan slijtage, blijft de getijdenkracht een factor tien tot twaalf te zwak.
Ook andere mechanismen schieten tekort. De stroming in Europa’s mantel (de laag onder de korst) zou in theorie breuken kunnen veroorzaken, maar zelfs in het meest optimistische scenario is die kracht honderden keren te zwak. En het krimpen van Europa’s binnenste door afkoeling? Daarvoor zou de rotsige kern met een hele kilometer moeten slinken voordat er iets zou breken.
Chemisch evenwicht: einde verhaal?
Zonder actieve breuken kan zeewater niet diep in de rotsbodem doordringen. Reacties tussen water en gesteente blijven dan beperkt tot hooguit de bovenste paar honderd meter. Na verloop van tijd bereikt die zone een chemisch evenwicht met de oceaan erboven en dan stopt de aanvoer van chemische energie.
Voor leven dat afhankelijk is van zulke chemische reacties is dat een probleem. Organismen die energie halen uit het mengen van vloeistoffen met verschillende chemische samenstellingen zouden op den duur zonder brandstof komen te zitten.
Is alle hoop verloren?
Niet helemaal. De onderzoekers wijzen op alternatieve energiebronnen die niet afhankelijk zijn van tektonische activiteit. Radioactief verval van uranium, thorium en kalium in het gesteente kan waterstof produceren, een proces dat radiolyse heet. Op aarde leven er micro-organismen in oude rotsformaties die precies dat doen, kilometers onder het aardoppervlak.
Of dit voldoende energie kan leveren voor een heel ecosysteem op Europa is nog onduidelijk. Maar het betekent wel dat de zoektocht naar leven niet per se ophoudt bij een geologisch stille zeebodem.
Europa Clipper gaat het uitzoeken
De NASA-missie Europa Clipper, die in 2024 is gelanceerd en in 2030 bij Jupiter aankomt, zal helpen om deze vragen te beantwoorden. Het ruimtevaartuig gaat onder andere meten hoe dik de ijslaag is, hoeveel warmte er vrijkomt door getijdenwerking en of er misschien waterpluimen uit de ijskorst spuiten die iets kunnen onthullen over de chemische samenstelling van de oceaan.
Toch zal zelfs deze missie wellicht geen definitief antwoord geven. Uiteindelijk zullen we de oceaan en misschien ooit de zeebodem rechtstreeks moeten onderzoeken om te weten of er leven is op Europa.
The smell of space has been described as similar to the smell of something cooking on a charcoal grill.
Rbkomar/Getty Images
Key Takeaways
Astronauts report that space has a distinct smell, often described as metallic or sweet.
These descriptions come from astronauts' experiences after returning from spacewalks and noticing the smell in the airlock, which suggests the scent clings to their suits and equipment.
The smell of space is thought to be due to the presence of polycyclic aromatic hydrocarbons, compounds that form in the dust and debris of space.
We all know space is empty, right? Most of space is completely absent of anything – not dust, not planets nor sun, not even air. So, why do many of the people who've been to space and spent time in it report that space has a smell?
It turns out that space does smell, and our solar system has a very particular smell. This is likely the result of several factors, but all are clear: Our corner of the universe is kind of stinky. If you're curious to learn what space smells like and why it smells that way, the explanation might surprise you.
While no astronaut has been unwise enough to unclasp and remove their helmet in the vacuum of space (which is very bad for longevity), astronauts have reported a smell upon returning from space. Specifically, many astronauts report different smells in the airlock after participating in spacewalks.
"The best description I can come up with is metallic; a rather pleasant sweet metallic sensation," wrote astronaut Don Pettit, according to Space.com. "It reminded me of my college summers where I labored for many hours with an arc welding torch repairing heavy equipment for a small logging outfit. It reminded me of pleasant sweet-smelling welding fumes. That is the smell of space." Pettit participated in several EVAs (extravehicular activities or spacewalks) during his NASA career, accumulating repeated experience with the smell.
Other astronauts have described it in similar yet varying ways: "burning metal," "a distinct odor of ozone, an acrid smell," "walnuts and brake pads," "gunpowder" and even "burnt almond cookie." Much like all wine connoisseurs smell something a bit different in the bottle, astronaut reports differ slightly in their "smelling notes" but have one thing in common: a burnt smell.
What might explain why space smells burnt? There are two possible explanations.
The Oxidation Explanation
One theory to explain the smell of space relates to the process that occurs in the airlock as astronauts return from space to the International Space Station or spacecraft they call home while orbiting Earth. During re-pressurization, the chemical reaction of oxidation occurs; atoms of oxygen in space attach to the astronaut's suit and float in during the de-pressurized time when the airlock is open and combine to form atmospheric oxygen (O2).
This process is similar to combustion without the flame and smoke – and smells similar too, which might explain the smoky, charred odor astronauts report.
The Stellar Explosion Explanation
A second hypothesis about what might explain the smell of space that astronauts report upon returning through the airlock relates to stellar explosions — that is, dying stars.
Though we've only been studying the night sky for a few centuries, the universe dates some 13.7 billion years old, and our solar system is estimated to be about 4.5 billion years old. This means that for literally billions of years before our solar system even formed, stars were being born and dying across the universe.
When stars die, it tends to be a dramatic affair, and this bombastic process creates a compound called polycyclic aromatic hydrocarbons (PAHs). PAHs are present throughout the solar system, including here on Earth; they can be found in some foods, coal and oil, among other materials. They also occur when coal, tobacco, wood, meat and other substances are burned. Perhaps part of the reason space has a distinctly burnt and charcoal smell is because it — like a grill on a summer evening — is emitting smelly PAHs.
Now That's Interesting
Outside our solar system, it's not as stinky! Other parts of the universe have other compounds and elements, which create different smells — though no human is likely to ever take a big whiff to confirm. For example, the dust cloud Sagittarius B2 has a high concentration of ethyl formate, which is the organic compound that gives both raspberries and rum their distinctive odors. If you love a good raspberry daiquiri, that's the corner of the universe for you!
A shocking admission by the CIA has just reopened the mystery surrounding 3I/ATLAS, the interstellar object speeding through our solar system.
Although NASA has claimed the object is an ordinary comet, an icy rock with a long tail of gas and dust, intelligence officials have refused to answer whether they investigated the possibility that 3I/ATLAS is an extraterrestrial craft.
In response to a November 2025 Freedom of Information Act (FOIA) request regarding the supposed comet, the CIA said it could 'neither deny nor confirm the existence or nonexistence of records' regarding 3I/ATLAS.
The federal government had maintained that the object showed no signs of harboring alien life or that it was an artificially constructed spacecraft since it was detected in July 2025.
However, the CIA still decided to provide what is known as a 'Glomar response.' It's a way for the government to say, 'We're not going to tell you if we have information or not, because even admitting that could reveal sensitive secrets.'
Harvard professor Avi Loeb has continued to challenge NASA's claims, highlighting that 3I/ATLAS has exhibited at least 12 strange behaviors that scientists have not been able to explain as natural occurrences.
Those anomalies include the object having a bright 'anti-tail' pointing in the opposite direction of a normal comet, course changes that defy the laws of gravity, and a nickel shell, which is a metal typically used by spacecraft to deflect heat.
'That this information is treated as sensitive enough to be classified by the CIA is surprising, given that NASA officials stated decisively at a press conference on November 19, 2025, that 3I/ATLAS is definitely a comet of natural origin,' Loeb said.
Amateur stargazers have taken clear images of the interstellar object 3I/ATLAS (Pictured) using common telescopes during its journey through the solar system
The CIA has released a statement neither confirming nor denying any investigations into 3I/ATLAS, complying with a November 2025 FOIA request
As 3I/ATLAS nears Jupiter on March 16, the Harvard physicist said the new revelations by the US intelligence community suggest the government has secretly investigated the possibility that the object is a hostile threat, as he theorized last year.
The Daily Mail has requested comment from both the CIA and NASA and is awaiting a response.
The FOIA request was submitted by UFO and government conspiracy researcher John Greenewald Jr, who noted in a post on X that he was filing an appeal to get a clearer answer from the CIA.
Greenewald Jr added that he has filed the same request for information regarding 3I/ATLAS with NASA and other US agencies and is still waiting for them to reply.
FOIA requests are part of US law that lets anyone, including citizens, journalists, and researchers, ask government agencies for documents or records on a specific topic.
The agency must give a response, but it can withhold revealing details if the information is classified for national security reasons or falls under certain exemptions.
'Very interesting, apparently CIA [director John] Ratcliffe knows something,' one person on social media alleged.
The new revelations have come months after NASA completely dismissed the possibility of 3I/ATLAS being extraterrestrial in origin, with space agency administrator Nicky Fox saying they've found nothing 'that would lead us to believe it was anything other than a comet.'
3I/ATLAS is projected to reach its closest point to Jupiter in March 2026 before leaving the solar system for good
However, NASA's November announcement created more doubt about the object's origins than it solved, as the agency was widely mocked for the blurry images it released of 3I/ATLAS.
Many critics quickly pointed out that amateur astronomers with common telescopes had been taking much clearer photographs of the alleged comet as it approached Earth in December, despite being over 200million miles from the object.
In comparison, NASA Mars orbiters were less than 20million miles away from 3I/ATLAS in early October 2025, but still only returned heavily pixelated images of the visitor, which caused some to claim it was a cover-up.
'NASA officials were encouraged to deliver the likely scientific interpretation, while at the same time, the serious consideration of a black swan event by the CIA was hidden from public view to prevent panic from taking hold for no good reason,' Loeb speculated in a statement published Monday.
A black swan event is a rare, totally unexpected happening that's highly unlikely but could have huge, world-changing consequences for the Earth.
In the case of the interstellar comet 3I/ATLAS, Loeb said if the tiny chance that the object was artificial alien technology turned out to be true, it would be a massive shock with enormous implications for humanity, including proving aliens exist.
The cryptic response from the CIA adds another layer to the eight-decade conspiracy theory UFO believers have had, claiming that the US government has been concealing what it knows about extraterrestrial life.
Just days after Greenewald Jr's FOIA request was submitted in November, the hit documentary 'The Age of Disclosure' was released, interviewing 34 US government, military, and intelligence officials about their knowledge of an alleged UFO cover-up.
Despite the speculation, the US military and federal government have said there has never been any physical proof that UFOs or beings from other planets exist.
Out in the depths of space, somewhere in between Mars and Jupiter, is a newly discovered asteroid that’s breaking records.
Astronomers have spotted a celestial rock the size of seven football pitches that is spinning faster than they’ve ever seen before.
The asteroid, named 2025 MN45, is 710 metres in diameter and completes a full rotation every 1.88 minutes.
The fact that it spins so rapidly has baffled experts, who say it must consist of solid rock in order to maintain its shape.
‘Clearly, this asteroid must be made of material that has very high strength in order to keep it in one piece as it spins so rapidly,’ Sarah Greenstreet, who leads the Rubin Observatory’s Solar System Science Collaboration’s Near-Earth Objects and Interstellar Objects working group, said.
‘We calculate that it would need a cohesive strength similar to that of solid rock.
‘This is somewhat surprising since most asteroids are believed to be what we call “rubble pile” asteroids, which means they are made of many, many small pieces of rock and debris that coalesced under gravity during Solar System formation or subsequent collisions.’
While it is currently out in the asteroid belt, hundreds of millions of kilometres away, asteroids and comets have previously been ‘nudged’ into Earth’s neighbourhood by the gravity of nearby planets.
This artist’s illustration depicts 2025 MN45 — the fastest-rotating asteroid with a diameter over 500 meters that scientists have ever found
The lightcurve of the asteroid - the y-axis shows the asteroid’s brightness, and the x-axis shows its phase, or where it is in its rotation
The sighting forms part of a much larger discovery, as scientists have detected 1,900 new asteroids cruising about our Solar System that have never been seen before.
Within this flurry are 19 super and ultra-fast rotating asteroids – with 2025 MN45 taking the new record for the fastest-spinning asteroid with a diameter over 500 meters that astronomers have found.
For their study, researchers collected data over the course of about 10 hours across seven nights in April and May of last year.
They used the Rubin Observatory’s LSST Camera – the largest digital camera in the world – to capture the night sky.
‘Discoveries like this exceptionally fast-rotating asteroid are a direct result of the observatory's unique capability to provide high-resolution, time-domain astronomical data, pushing the boundaries of what was previously observable,’ Regina Rameika, from the US Department of Energy, said.
As asteroids orbit the Sun, they also rotate at a wide range of speeds, the researchers explained.
These spin rates not only offer clues about the conditions of their formation billions of years ago but also tell us about their internal composition and evolution over their lifetimes.
In particular, an asteroid spinning quickly may have been sped up by a past collision with another asteroid, suggesting that it could be a fragment of an originally larger object.
Most asteroids can be found orbiting our Sun between Mars and Jupiter within the main asteroid belt
An illustration of the main asteroid belt, orbiting the Sun between Mars and Jupiter, where asteroid 2025 MN45 can be found
This image, one of the first released by Rubin Observatory, exposes a Universe teeming with stars and galaxies — transforming seemingly empty, inky-black pockets of space into glittering tapestries for the first time
‘Fast rotation also requires an asteroid to have enough internal strength to not fly apart into many smaller pieces, called fragmentation,’ the team said in a release.
‘Most asteroids are ‘rubble piles’, which means they are made of many smaller pieces of rock held together by gravity, and thus have limits based on their densities as to how fast they can spin without breaking apart.
‘For objects in the main asteroid belt, the fast-rotation limit to avoid being fragmented is 2.2 hours; asteroids spinning faster than this must be structurally strong to remain intact.
‘The faster an asteroid spins above this limit, and the larger its size, the stronger the material it must be made from.’
Within the main asteroid belt are space rocks ranging in size from 530km (329 miles) to just 10 metres (33 feet) in diameter.
‘Sometimes, asteroids and comets are nudged into Earth’s neighbourhood by the gravity of nearby planets,’ NASA says.
However, they explained that it is ‘highly unlikely’ an asteroid large enough to cause widespread damage will impact Earth for the next 100 years or more.
Currently, NASA would not be able to deflect an asteroid if it were heading for Earth but it could mitigate the impact and take measures that would protect lives and property.
This would include evacuating the impact area and moving key infrastructure.
Finding out about the orbit trajectory, size, shape, mass, composition and rotational dynamics would help experts determine the severity of a potential impact.
However, the key to mitigating damage is to find any potential threat as early as possible.
NASA and the European Space Agency completed a test which slammed a refrigerator-sized spacecraft into the asteroid Dimorphos.
The test is to see whether small satellites are capable of preventing asteroids from colliding with Earth.
The Double Asteroid Redirection Test (DART) used what is known as a kinetic impactor technique—striking the asteroid to shift its orbit.
The impact could change the speed of a threatening asteroid by a small fraction of its total velocity, but by doing so well before the predicted impact, this small nudge will add up over time to a big shift of the asteroid's path away from Earth.
This was the first-ever mission to demonstrate an asteroid deflection technique for planetary defence.
The results of the trial are expected to be confirmed by the Hera mission in December 2026.
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Over mijzelf
Ik ben Pieter, en gebruik soms ook wel de schuilnaam Peter2011.
Ik ben een man en woon in Linter (België) en mijn beroep is Ik ben op rust..
Ik ben geboren op 18/10/1950 en ben nu dus 75 jaar jong.
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