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.
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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!!!
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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.
03-03-2026
Things on Mars That Look Like They Shouldn’t Be There
Things on Mars That Look Like They Shouldn’t Be There
Mars has always captivated our imagination, but modern space exploration has made it even more intriguing. High-resolution Mars anomalies images from NASA’s rovers and orbiters often reveal formations that resemble familiar objects—from faces to doorways—leading to fascinating debates.
While most of these anomalies have logical geological explanations, they spark curiosity about what lies beneath the Red Planet’s dusty surface. Here are 15 of the strangest things spotted on Mars that look like they shouldn’t be there.
1. The “Face on Mars”
Photo Credit: Wikipedia
One of the most iconic Mars anomalies images , the “Face on Mars,” was first photographed by NASA’s Viking 1 orbiter in 1976. The image appeared to show a massive humanoid face, sparking decades of speculation about alien civilizations.
Later, high-resolution images from the Mars Reconnaissance Orbiter revealed it as a natural mesa with shadows creating facial illusions. This phenomenon is a classic example of pareidolia—our brain interpreting random patterns as familiar shapes. Even though it’s been debunked, the face remains a pop culture symbol of extraterrestrial mystery. (NASA)
2. The “Doorway” Rock Formation
Photo Credit: ChatGPT
In 2022, NASA’s Curiosity rover captured an image resembling a doorway carved into a cliffside. The feature sparked theories about ancient Martian structures. However, scientists clarified that it’s likely the result of natural fracturing and erosion in the rock.
This “doorway” measures only a few centimeters high, ruling out the possibility of it being an entrance. Its clean, rectangular shape is still fascinating, highlighting how wind and seismic activity can mimic artificial designs. (BBC News)
3. The “Spoon” in Gale Crater
Photo Credit: THE SUN
In 2015, images from the Curiosity rover revealed a rock that appeared to be a floating spoon. Its thin, curved shape made it an internet sensation. Scientists explain it as a rock formation shaped by wind erosion, with its thin neck eroding faster than its broader “bowl” area.
While it’s not actually levitating, the angle of the photo enhances the illusion. Such formations are examples of ventifacts—rocks sculpted by wind-driven sand over long periods. (NASA Jet Propulsion Laboratory)
4. The “Blueberries” of Meridiani Planum
Photo Credit: NASA
In 2004, NASA’s Opportunity rover discovered tiny, spherical formations nicknamed “blueberries.” These hematite-rich concretions are formed by the action of mineral-laden water, suggesting Mars once had conditions suitable for life.
Their abundance and uniformity puzzled scientists initially, but their composition provides evidence of ancient water activity. These “blueberries” are now a key piece in understanding Mars’ wetter past. (NASA Science)
5. A “Pyramid” Structure
Photo Credit: BOW
A pyramid-like rock was photographed by Curiosity in 2015, leading some to claim evidence of ancient Martian architecture. However, geologists point out that such shapes can form naturally through fracturing and erosion.
The sharp edges and triangular profile are coincidental, though they fuel imaginative theories about intelligent design. This formation highlights how our pattern-recognition instincts often outpace scientific explanations. (National Geographic)
6. The “Legless Lizard” Rock
Photo Credit: NASA
In 2013, a Curiosity image seemed to show a small lizard-like creature on Mars. This fueled online claims of living organisms. NASA scientists quickly dismissed these as illusions caused by rock shadows and shape pareidolia.
Close analysis revealed it was nothing more than an oddly shaped rock. Such sightings underscore the human tendency to project familiar life forms onto alien landscapes. (NASA)
7. The “Cannonball” Spheres in Gale Crater
Photo Credit: NASA
Curiosity discovered nearly perfectly spherical rocks in 2016, resembling cannonballs scattered across the Martian surface. These are actually concretions—hard mineral masses formed within sedimentary layers when groundwater deposits minerals over time.
Their near-perfect shape makes them stand out in the rugged Martian terrain, adding to the planet’s mysterious geological story. The spheres provide insights into Mars’ aqueous past, helping scientists piece together how water once influenced its geology. (Space.com)
8. The “Thigh Bone” Rock Illusion
Photo Credit: SPACE
In 2014, a rock shaped like a human femur was spotted by Curiosity. Its bone-like appearance fueled speculation about Martian fossils and ancient creatures.
However, NASA scientists attribute it to erosion and fracturing, emphasizing that Mars’ surface processes can produce surprisingly familiar shapes. This peculiar resemblance reinforces how visual illusions often spark theories about alien life. (NASA)
9. The “Stonehenge” Circle of Rocks
Photo Credit: ChatGPT
In 2018, satellite images revealed a circular arrangement of rocks resembling Earth’s Stonehenge, baffling some observers. This feature, located in the Mawrth Vallis region, is believed to be a natural consequence of impact cratering and weathering.
The ring formation, while eye-catching, serves as a reminder that natural processes can mimic intentional design, leading to fascinating debates about its origins. (The Guardian)
10. The “Tree Stump” Rock Formation
Photo Credit: METRO
In 2016, Curiosity photographed a rock resembling a fossilized tree stump, leading some to argue it hinted at ancient vegetation. Experts explained it as an eroded mudstone outcrop shaped by sedimentary processes.
Its layered appearance may suggest ancient water-related activity, but there’s no evidence it was biological. The structure remains one of the most visually striking finds so far. (NASA JPL)
11. The “Bear Face” Crater Image Discovery
Photo Credit: NASA
In 2023, the Mars Reconnaissance Orbiter captured an image of a crater resembling a bear’s face. Its “eyes” are two smaller craters, and the “snout” is a collapsed mound shaped over time.
This example of pareidolia shows how our minds interpret random arrangements as recognizable images. Such formations are fun yet scientifically significant, revealing the planet’s dynamic and complex surface evolution. (Smithsonian Magazine)
12. The “Glass Tubes” Dune Illusion Explained
Photo Credit: ScholarWorks
Images from Mars Global Surveyor once appeared to show translucent, tube-like structures on the surface, leading to wild theories about Martian transport systems or pipelines.
Later analysis revealed these were rows of sand dunes illuminated at certain angles, giving the illusion of tubes. This optical effect underscores the challenges of interpreting alien landscapes from orbital imagery, often creating misleading impressions. (NASA)
13. The “Crab Monster” Rock Shadow Appearance
Photo Credit: ChatGPT
In 2015, Curiosity captured an image that many claimed looked like a giant crab hiding in a cave. NASA quickly explained this as a rock formation created by shadows and lighting effects interacting with rough terrain.
This example highlights how pareidolia thrives when viewing low-resolution or shadowed imagery in alien environments, sparking viral discussions and conspiracy theories online. (National Geographic)
14. The “Fossilized Spine” Rock Feature Illusion
Photo Credit: ScholarWorks
Another 2017 rover image showed what looked like a segmented spine protruding from the ground. Some speculated it might be evidence of past Martian life or ancient fossilized remains.
However, geologists identify it as a common type of sedimentary rock with fractures giving it a spine-like appearance. While intriguing, no biological explanation holds up under detailed scientific review or peer analysis. (Space.com)
15. The “Wheel Tracks” Natural Grooves Explained
Photo Credit: NASA
In some rover images, natural grooves in Martian terrain have been mistaken for vehicle tracks from unknown sources or previous explorers. These linear features are actually caused by repeated wind erosion or dried channels carved over long periods.
Comparing them with actual rover tracks reveals significant differences in depth and uniformity, proving their natural origin beyond reasonable scientific doubt. (NASA)
Relatistic representation of a Dyson swarm. Credit - Віщун / Wikimedia Commons
Ever since physicist Freeman Dyson first proposed the concept in 1960, the “Dyson sphere” has been the holy grail of techno-signature hunters. A highly advanced civilization could build a “sphere” (or, in our more modern understanding, a “swarm” of smaller components) around their host star to harvest its entire energy output. We know, in theory at least, that such a swarm could exist - but what would it actually look like if we were able to observe one? A new paper available in pre-print on arXiv, and soon to be published in Universe from Amirnezam Amiri of the University of Arkansas digs into that question - and in the process discloses the types of stars that are the most likely to find them around.
Perhaps unsurprisingly, one of those types is a Red Dwarf. The most abundant type of stars in the Milky Way, they burn through their nuclear fuel incredibly slowly making them extremely long lived. With estimated lives in the trillions of years - far longer than the current lifetime of the universe - they are also relatively small compared to our own Sun. A Dyson swarm could be built around 0.05 to 0.3 AU away from its surface, with relatively low cost of material.
White dwarfs are arguably even better for material costs, and represent the second type of star that it’s worth tracking. These are compact, dead remnants of stars like our Sun, which have shrunk down to have incredibly small radii - around 1% of their original star. In this scenario, a Dyson swarm could be built just a few million kilometers away from the surface of the star, alleviating much of the engineering challenge of build a supermassive structure around a larger star. They also radiate energy steadily for billions of years, essentially creating an effective long-lived power source.
*The H-R diagram used to classify stars.
Credit - ESO*
But what would stars surrounded by such megastructures actually look like? Astronomers typically use a tool called the Hertzsprung-Russell (H-R) diagram to classify stars based on their temperature and luminosity. However, since a Dyson sphere would block all of a star’s natural light, it would completely change where on the diagram it would fall. Energy can neither be created nor destroyed, so the sphere itself would have to emit the exact same amount of radiation away from itself as the star is putting into it. It just does it in the form of heat, or infrared light instead. So a Dyson sphere can really be thought of as a shell that absorbs a star’s light, does something useful with that energy, and then emits it as heat.
In doing so, it is shifting the location of the star entirely to the right - where lower temperatures are mapped on the diagram. The luminosity itself doesn’t change at all, it is simply shifted to the infrared, and since H-R diagrams use bolometric luminosity (i.e. the luminosity over all of the spectra), it would appear in the same vertical place on the diagram as whatever its host star is, whether that’s a red or white dwarf.
But the key take away is how much further on the right the star would go. A typical red dwarf, which inhabits the lower right hand corner of a H-R diagram, has a surface temperature of around 3000K degrees. A Dyson sphere surrounding a star would have a temperature down to 50K - two orders of magnitude lower. There are no natural stars in this area, making any such object highly interesting as a potential Dyson swarm candidate.
Fraser explains the concept of a Dyson Sphere.
One further factor contributing to the possibility of an object being a Dyson swarm is a lack of dust. A star without a Dyson sphere would typically show a spectral line for silicate emission that is commonly associated with dusky disks. However, radiator panels don’t have any dust surrounding them, so they would look remarkably “clean” to a spectrograph monitoring them.
One thing to note - in the “swarm” methodology, there would likely be gaps between some of the solar collectors, or varying thickness in certain parts of the swarm. This is intended to make the material requirements actually physically possible - modern calculations show that, even with relatively small radii, an actual full Dyson sphere is physically impossible. In the case where there were these small gaps, the star would behave exceedingly erratically, with non-natural light curves as the structure rotates.
Since infrared is the specialty of the James Webb Space Telescope, it is well placed to monitor for these kinds of structures. But even older telescopes like WISE are being actively used to search for them. In May 2024, a paper highlighting work from Project Hephaistos identified seven strong Dyson sphere candidates (all red dwarfs) out of a catalogue of 5 million stars. One was eliminated as a possible source, as there was a supermassive black hole aligned perfectly in the background around the star, explaining the anomalous readings. But that still leaves five more potential candidates that are worth some closer observation. This new paper will add another tool to astronomers’ understanding of what to search for to one day find one of these elusive technosignatures.
A laser 3D printing method, tested by researchers at OSU, could lead to resilient, stable structures on the Moon. Credit: ESA
Through the Artemis Program, NASA hopes to establish a permanent human presence on the Moon in its southern polar region. China, Russia, and the European Space Agency (ESA) have similar plans, all of which involve building bases near the permanently shadowed regions (PSRs) - i.e., craters that contain water ice - that dot the South Pole-Aitken Basin. For these and other agencies, it is vital that these bases be as self-sufficient as possible since resupply missions cannot be launched regularly and take several days to arrive.
Therefore, any plan for a lunar base must come down to harvesting local resources to meet the needs of its crews as much as possible - a process known as In-Situ Resource Utilization (ISRU). In a recent study, researchers at The Ohio State University (OSU) proposed using a specialized laser-based 3D printing method to turn lunar regolith into hardened building material. According to their findings, this method can produce durable structures that withstand radiation and other harsh conditions on the lunar surface.
The importance of ISRU for human exploration has prompted the rapid development of additive manufacturing systems - aka 3D printing. These systems have proven effective at fabricating tools, structures, and habitats, effectively reducing dependence on supplies delivered from Earth. Developing such systems for long-duration missions is one of the most challenging aspects of the process, as they must be engineered to operate in the extreme environment on the Moon. This includes the lack of an atmosphere, massive temperature variations, and the ever-present problem of Moon dust.
Scientists use two types of lunar regolith for their experiments and research: Lunar Highlands Simulant (LHS-1) and Lunar Mare Simulant (LMS-1). As part of their research, the team used LHS-1, which is rich in basaltic minerals, similar to rock samples obtained by the Apollo missions. They melted this regolith with a laser to produce layers of material and fused them onto a base surface of stainless steel or glass. To assess how well these objects would fare in the lunar environment, the team tested their fabrication process under a range of different environmental conditions.
One thing they noticed was that the fused regolith adhered well to alumina-silicate ceramic, possibly because the two compounds form crystals that enhance heat resistance and mechanical strength. This revealed that the overall quality of the printed material is largely dependent on the surface onto which the regolith is printed. Other environmental factors, such as atmospheric oxygen levels, laser power, and printing speed, also affected the stability of the printed material. As Xu explained in an OSU News release:
By combining different feedstocks, like metal and ceramics, in the printing process, we found that the final material is really sensitive to the environment. Different environments lead to different properties, which directly affect the mechanical strength and the thermal shock resistance of certain components. There are so many applications that we’re working toward that with new information, the possibilities are endless.
*Astronauts collecting samples on the lunar surface as part of NASA's Artemis Program.
Credit: NASA*
Deployed to the Moon's surface, this process could help build habitats and tools that are strong, resilient, and capable of handling the lunar environment. This has the added benefit of increasing independence from Earth, which is key to realization long-duration missions on the Moon. In addition to assisting astronauts exploring the Moon in the near future (as part of NASA's Artemis Program), this technology could also lead to resilient habitats that will enable a long-term human presence on the Moon, Mars, and beyond.
However, there are several unknown environmental factors that could limit the effectiveness of these systems on other worlds, and more data is needed before they can be addressed. In their study, the team suggests that instead of being powered by electricity, future scaled-up versions of their method could rely on solar or hybrid power systems. Nevertheless, the potential for space exploration is clear, and the technology also has applications for life here on Earth. Sarah Wolff, an assistant professor in mechanical and aerospace engineering and a lead author on the study, explained:
There are conditions that happen in space that are really hard to emulate in a simulant. It may work in the lab, but in a resource-scarce environment, you have to try everything to maximize the flexibility of a machine for different scenarios. If we can successfully manufacture things in space using very few resources, that means we can also achieve better sustainability on Earth. To that end, improving the machine’s flexibility for different scenarios is a goal we’re working really hard toward.
As the saying goes, "Solving for space solves for Earth." In environments where materials and resources are limited, laser-based 3D printing is one of several technologies that could support sustainable living. This applies equally to extraterrestrial environments and to regions on Earth experiencing the effects of Climate Change.
Image of Milnesium tardigradum in active state (Credit : Schokraie E, Warnken U, Hotz-Wagenblatt A, Grohme MA, Hengherr S, et al. (2012) - Schokraie E, Warnken U, Hotz-Wagenblatt A, Grohme MA, Hengherr S, et al. (2012))
You could fit about a dozen of them across the full stop at the end of this sentence. Under a microscope they look like tiny eight legged bears shuffling around in slow motion. They have been frozen, boiled, irradiated, sent into the vacuum of open space and brought back alive. Scientists have been studying them for over two hundred years and they still have the capacity to astonish. Their name is tardigrade, though most people know them by the rather more charming nickname of water bears. And right now, they might be one of our best tools for figuring out how to survive on Mars.
A team of researchers from Penn State University has just published a study that used tardigrades in a genuinely novel way, not to test how tough they are, but to test how tough Mars is. Specifically, they wanted to understand how the planet's regolith, the loose mineral deposits that cover the Martian surface rather like soil covers our own, would interact with living animals. Could it ever be adapted to support plant growth for future human explorers? And could it actually help protect the planet from contamination that humans might inadvertently bring with them?
Simulated Martian regolith
(Credit : Z22)
To find out, they mixed active tardigrades with two different simulated Martian soils, both designed to precisely replicate the mineral and chemical composition of regolith sampled by NASA's Curiosity Rover from a region called the Rocknest deposit, inside the Gale Crater.
The first simulant, known as MGS-1 was designed to represent the Martian surface broadly and yielded terrible results. Within just two days, the tardigrades showed severely reduced activity. For an animal that routinely shrugs off the vacuum of space, that is extraordinary. The second simulant was still inhibitory but far less damaging, which itself tells researchers something important about exactly which aspects of Martian soil pose the greatest risk.
Then came the surprise. When the team rinsed the MGS-1 simulant with water before introducing fresh tardigrades, the damage almost vanished entirely. Something in the soil, possibly dissolved salts or another soluble compound, was responsible for the harm, and water washed it away. The same property that made the regolith so hostile to life also makes it a potential natural barrier against Earthly contamination. Mars, in a sense, may have its own built in defence system.
This self-portrait of NASA's Curiosity Mars rover shows the vehicle at the "Big Sky" site, where its drill collected the mission's fifth taste of Mount Sharp
(Credit : NASA)
This matters enormously for what scientists call planetary protection, the internationally agreed principle that we should not contaminate other worlds with Earth life, and equally should not bring alien contamination back home. If Martian soil is naturally hostile to Earth organisms, that provides a degree of reassurance. But equally, if a simple rinse with water can neutralise that hostility, then future colonists might be able to process regolith to grow food after all.
Water, of course, is precious on Mars, which means washing soil on an industrial scale is not a straightforward solution. But knowing the problem can be solved at all is a significant step forward. As the researchers put it, they are beginning to tease apart the components of an enormously complex system, one piece at a time.
The water bears have survived everything Earth could throw at them for hundreds of millions of years. It turns out they may be exactly the right animal to help us understand whether Mars will ever be ready to welcome us.
An artist's concept depicts a greenhouse on the surface of Mars. Plants are growing with the help of red, blue, and green LED light bars and a hydroponic cultivation approach. Other methods using soil simulants should also contribute to long-term food production on the Moon and Mars. Image credit: SAIC
In the future, farmers on the Moon and Mars will have a big challenge: how to grow healthy food in two extremely unhealthy environments. That's because the soil on both worlds isn't at all hospitable to plants and animals. Neither are other conditions. Both are irradiated worlds, Mars has a thin atmosphere and the Moon has none at all. So, how will future colonists on either world grow their food?
We could look toward the example shown by Matt Damon in "The Martian". There, a stranded Marsnaut figures out how to grow potatoes using his own sewage, which turns out to be do-able according to experiments run by the International Potato Center and NASA few years ago. More recently, researchers led by Harrison Coker of Texas A&M worked with a team at NASA, tested a solution of recycled sewage products and how they interacted with simulated lunar and Mars regolith (soil). The NASA team, headquartered at Kennedy Space Center, is taking a deep look at what are called bioregenerative life support systems (BLiSS). These bioreactors and filters turn an artificial form of sewage into a solution rich in the kinds of nutrients that plants need to thrive. This work has immediate implications for people who will be living and working on the Moon and Mars in the future. That's because people can easily furnish the waste products needed. With the upcoming Artemis missions to the Moon, the question of food production is assuming a high priority for long-term inhabitants.
“In lunar and Martian outposts, organic wastes will be key to generating healthy, productive soils, said Coker, the first author on a study of such systems. “By weathering simulant soils from the Moon and Mars with organic waste streams, it was revealed that many essential plant nutrients can be harvested from surface minerals.”
A simulated lunar greenhouse at NASA Kennedy Space Center is helping scientists solve the problem of growing food on the Moon, and ultimately Mars.
Courtesy NASA.
What Do Plants Need?
The plant life on Earth needs a complex set of nutrients to thrive. For example, corn needs a great deal of nitrogen. Peas like potassium and phosphorus. Potatoes like both phosphorus and nitrogen. And, all planets need water. The researchers looked at what it would take to "enrich" Martian and lunar regoliths. It turns out, they need a lot. That's because the soils are irradiated and in the case of Mars, rich in sulfur, ferric oxide, silicon dioxide, and magnesium. It's also laced with high levels of perchlorates, which are toxic.
The first inhabitants of these worlds will need to bring their own food and sewage systems, and then work on making the local soils habitable for plants. That will take time and a lot of work, in addition to all the other projects they'll need to fulfill, such as exploration and habitat building.
Of course, the future inhabitants could rely on hydroponics for a growth medium, and there have been a great many studies of such water-based systems. However, you do need a lot of water and the nutrient loads need to be quite high to produce food in great quantities. On the Moon, at least, astronauts could send back to Earth for supplies, but that's going to be expensive and time-consuming. So, it's likely that the first sets of explorers will depend on food from "home". However, that can't be a permanent solution, which is why scientists are looking at ways to make local soils good for farming in the long run.
*Studies of food growth in space go back many years. A variety of red potatoes called Norland were grown in the Biomass Production Chamber inside Hangar L at Cape Canaveral Air Force Station in Florida during a research study in 1992.
Credit: NASA*
Better Farming Through Sewage and Chemistry
In the research led by Coker and the folks at NASA, scientists combined the BLiSS effluent they created with simulated Martian or lunar regolith (each called a simulant). Then, they stored the two different solutions in a shaker for 24 hours. The goal was to determine if the BLiSS effluents could essentially "weather" the regolith and provide a nutrient-rich growing solution.
It turns out that the weathered simulants supplied large amounts of essential plant nutrients. They including sulfur, calcium, and magnesium, and other metals, when interacting with both water and BLiSS solutions. In addition, looking at the simulant particles under a microscope revealed weathered features such as tiny pits forming in the lunar simulant and the Martian simulant becoming covered in nanoparticles. Both helped make the sharp minerals in the simulant less abrasive, showing successful weathering and a step toward a more soil-like material.
So, is recycling human sewage the solution for better off-world gardens? Not quite. Despite promising initial results, the next steps would need to include tests on actual lunar and Martian regoliths. They're quite different from the simulants the scientists tested. It's a good start, though, and provides crucial insights into a process that will be critical for sustaining human colonies in outer space. It may not be long before lunar citizens are snacking on watercress sandwiches and Mars colonists are growing their own corn, beans, and yes, potatoes, thanks to their own effluent products.
Artist's impression of an Orion spacecraft and Starship HLS rendezvousing in lunar orbit. Credit: Lockheed Martin
Earlier today, NASA announced that it would be increasing the cadence of its missions to meet its objectives under the Artemis Program. It is also making changes to its mission architecture to include a standard vehicle configuration and undertake one surface landing every year after 2027. In real terms, this means that a lunar landing will not take place as part of Artemis III in 2027, but during Artemis IV, currently scheduled for 2028. Instead, Artemis III will involve a rendezvous in Low Earth Orbit (LEO) to test the systems and operations for the first lunar landing in over sixty years.
The announcement came during a news conference at NASA's Kennedy Space Center, amid discussions about the status of the Artemis II mission. As Isaacman and other NASA officials stated, the agency now envisions an orbital rendezvous with a crewed Orion spacecraft and either the Starship HLS or Blue Origin's Blue Moon lander. This means that Artemis III* will mirror the Apollo 9* mission, which took place in March 1969 and was the first test of the Apollo Lunar Module in space, including docking maneuvers in LEO.
Per the agency's statement, the mission will also include in-space tests of the docked vehicles, integrated life support, communications, propulsion, and the new Extravehicular Activity (xEVA) spacesuits. Further details on this test flight will be released pending completion of detailed reviews between NASA and its commercial partners, and it was indicated that updates will be made soon. As NASA Administrator Jared Isaacman explained, the key considerations here are safety, competition, and "standardization":
NASA must standardize its approach, increase flight rate safely, and execute on the President’s national space policy. With credible competition from our greatest geopolitical adversary increasing by the day, we need to move faster, eliminate delays, and achieve our objectives. Standardizing vehicle configuration, increasing flight rate and progressing through objectives in a logical, phased approach, is how we achieved the near-impossible in 1969 and it is how we will do it again.
*Artist's impression of NASA astronauts operating on the lunar surface, as part of the Artemis Program.
Credit: NASA*
What to make of this news? At face value, these sound like perfectly sensible considerations, but there are undeniable concerns that could be motivating this switch-up as well.
Delays?
For starters, this news comes about six months after the former acting-Administrator Sean Duffy announced that NASA was reopening the competition for a Human Landing System (HLS), a contract awarded exclusively to SpaceX in 2021. However, delays with the Starship's development have led NASA to conclude that the HLS will not be ready in time for Artemis III. This includes an in-orbit refueling demonstration, currently planned for later this year.
But between the Starship's current payload limits and fuel leaks and engine failures that have led to five out of eleven prototypes being lost, this is unlikely to happen. While the Starship is intended to launch between 100 and 150 metric tons (110 and 165 US tons) to LEO in its fully-reusable form, tests with the Block 2 prototype have been limited to about 35 metric tons (38.5 US tons). To perform in-orbit refueling, SpaceX will need to launch multiple refueling tankers into orbit in advance to fuel the proposed orbital depot fully.
Given the Starship's fuel capacity of up to 1,500 metric tons (1650 US tons), this means 10 to 15 tankers will need to launch to refuel one HLS fully. Even if, as Elon has suggested, it can perform its mission objectives with only half a tank of liquid methane and liquid oxygen, that means five to eight tankers will be needed. But only if they can reach their full payload capacity, something the company hopes to remedy with the Block 3 version of the Starship. The first test flight of this latest prototype is scheduled for April 7th, 2026. Significant tests will need to take place before SpaceX can conduct the multiple launches needed for a refueling demonstration.
Meanwhile, Blue Origin has been making great strides in developing its New Glenn orbital launch vehicle. Although the vehicle has launched only twice, the second stage has managed to reach orbit both times without incident. In fact, the first launch placed its payload (the Blue Ring pathfinder) in a Medium-Earth Orbit (MEO) while the second deployed NASA's Escape and Plasma Acceleration and Dynamics Explorers (ESCAPADE) mission at the Earth-Sun L2 Lagrange Point.
*The Artemis II rocket on Launch Pad 39A at NASA's Kennedy Space Center.
Credit: NASA*
Under the circumstances, it is understandable why NASA is taking a more measured approach and pushing the date of the lunar landing mission forward.
No New Configurations
Another keyword in the statement is "standardization," referring to the configuration of the Space Launch System (SLS). Previously, NASA planned to upgrade the SLS design after Artemis III, moving from the Block 1 configuration to Block 1B. The first three SLS launches will rely on the former, with the Interim Cryogenic Propulsion Stage (ICPS), which provides propulsion to the Orion spacecraft after the solid rocket boosters and core stage are jettisoned, as part of the upper stage. The Block 1B version was to feature a larger Exploration Upper Stage (EUS), a four-engine liquid hydrogen/liquid oxygen propulsion system.
The purpose of this decision is to enable a faster launch cadence of a mission per year, something that Bill Gerstenmaier, the former Associate Administrator for Human Exploration and Operations, recommended in 2016. It also mirrors what NASA accomplished during the Apollo Era, where eight launches (Apollo 8 to 14) were conducted between 1968 and 1972. NASA Associate Administrator Amit Kshatriya indicated as much, referencing Apollo by name:
We are looking back to the wisdom of the folks that designed Apollo. The entire sequence of Artemis flights needs to represent a step-by-step build-up of capability, with each step bringing us closer to our ability to perform the landing missions. Each step needs to be big enough to make progress, but not so big that we take unnecessary risk given previous learnings. Therefore, we want to fly the landing missions in as close to the same Earth ascent configuration as possible – this means using an upper stage and pad systems in as close to the ‘Block 1’ configuration as possible.
Politics and Cutbacks
In its statement, NASA also mentioned its recently announced workforce directive as vital to the "acceleration" of the Artemis Program. The directive is intended to "rebuild core competencies in the civil servant workforce," which is a rather telling statement. On the one hand, it sounds reminiscent of Isaacman's past comments, in which he repeatedly criticized NASA's "bureaucratic" nature and how it has prevented progress. This could mean that "rebuilding core competencies" is merely an extension of his expressed desire to impose private-sector thinking on a public agency.
On the other hand, it could be a veiled reference to the recent cutbacks and layoffs NASA has been forced to contend with. In addition to a 25% reduction in overall funding for FY 2026, NASA experienced significant workforce reductions, with over 4,000 employees lost through buyouts and attrition. This has left more than 40 missions in danger, including Mars Odyssey, MAVEN, and OSIRIS-APEX. The same budget request also included the cancellation of the Space Launch System (SLS), the Orion spacecraft, and the Lunar Gateway, all vital aspects of NASA's long-term vision for a "sustained program of lunar exploration and development."
It also called for the cancellation of the Demonstration Rocket for Agile Cislunar Operations (DRACO) mission, a joint project initiated by NASA and DARPA in 2023. These decisions were enacted under Duffy, whom Isaacman got into a bit of a row with in November 2025 due to the leak of the "Project Athena" document, which outlined what Isaacman originally planned to do as NASA's Administrator. Eric Berger of Ars Technica, writing at the time, indicated it was possible Duffy himself leaked the document to "hold onto his job" as acting Administrator.
In essence, the leaked version of the plan appeared to be intended to lay the cancellations and layoffs at Isaacman's feet. According to Berger, the 62-page document (Isaacman stressed that the original was over 100 pages long) does not bear this out. As Isaacman stated in a post on X (dated Nov. 4th, 2025), "This plan never favored any one vendor, never recommended closing centers, or directed the cancellation of programs before objectives were achieved. The plan valued human exploration as much as scientific discovery."
Perhaps, then, this decision is motivated by a genuine desire to get NASA back on track and to restore the programs affected by measures enacted under Duffy, with the blessing of the current administration.
Competition
This certainly makes sense in light of what Isaacman said about competition from "our greatest geopolitical adversary" - aka China. For years, China has been making significant progress in its crewed and robotic space programs, and its plans for the future are nothing if not ambitious. But it is the progress they've seen in their lunar program that has left many analysts and observers in the West concerned that China could reach the Moon before NASA. This includes the development of the Long March-10 super-heavy launch system and the Mengzhou spacecraft, both of which passed a key launch test less than two weeks ago.
According to their current plan, the Mengzhou spacecraft and Lanyue lunar lander will launch separately aboard two Long March-10 rockets. This mission is slated for 2030 and is part of China's larger effort to develop an International Lunar Research Station (ILRS) in the Moon's southern polar region to rival NASA's Artemis Program.
Much like Elon Musk's recent announcement that SpaceX was pivoting to focus on the Moon instead of Mars, there are many common-sense reasons for these decisions. However, the context in which they occurred and additional incentives certainly warrant exploration. One thing is for certain: NASA has experienced repeated delays since the Moon-to-Mars mission architecture was first undertaken over 20 years ago, due to limited budget, shifting priorities, and needless shake-ups.
In the meantime, NASA continues to work on the *Artemis II* mission, which has been delayed again until April due to a helium flow issue that engineers identified in the ICPS during the latest wet dress rehearsal. After the Artemis II was rolled back into the Vehicle Assembly Building (VAB), the team immediately began working to resolve the issue. They're also preparing for several actions, including replacing batteries in the flight termination system, conducting end-to-end testing to meet range safety requirements, and more.
Jupiteris the largest planet in the solar system and has proudly boasted about this since time immemorial, with its scientific confirmation occurring by Galileo Galilei in 1610. It was later found that Jupiter has a bulging equator caused by its rapid rotation, turbulent atmosphere, and complex interior mechanisms despite its massive size, and scientists have even measured its “waistline” down to a tenth of a kilometer. Now, imagine being the largest planet in the solar system and you’re told you’re not as big as you thought. Where probably most humans would be thrilled to find this out, how do you respond if you’re Jupiter?
We might never know how Jupiter feels about being slimmer. But a team of international researchers led by the Weizmann Institute of Science in Israel are happy to explain how they feel about this incredible finding, which was recently published in *Nature Astronomy*. To accomplish this, the team used a combination of data obtained from NASA’s past missions of Pioneer 10 and Pioneer 11, which visited Jupiter in December 1973 and December 1974, respectively, Voyager 1 and Voyager 2, which visited Jupiter in March and July of 1979, respectively, and the currently active Juno spacecraft, which arrived at Jupiter in July 2016.
While the Pioneer and Voyager missions used a technique called radio occultation to measure Jupiter’s radius, with Voyager using an improved method, Juno used a combination of multi-angle radio occultation and gravity science to obtain its measurements.
Radio occultation involves using radio waves to estimate Jupiter’s size, with Pioneer using this method when the radio waves between itself and Earth were “cut off” as the spacecraft passed behind Jupiter. This not only estimating its radius but also confirmed Jupiter had an equatorial bulge, which was first proposed by Giovanni Cassini in 1666. Voyager improved this method by using radio waves to study Jupiter’s atmosphere, with the measured radius being the official measurement since then. Finally, Juno’s multi-angle radio occultation involves dividing Jupiter into “slices”, while the gravity science method involves measuring the tiny speed changes the spacecraft encounters that is produced by Jupiter’s massive gravity.
In the end, the researchers provided some of the most accurate measurements of Jupiter’s polar and equator radius ever. This includes a polar radius of 66,842 km (41,533 mi), an equatorial radius of 71,488 km (44,420 mi) and a mean radius of 69,886 km (43,487 mi), which are 12 km (7.4 mi), 4 km (2.5 mi) and 8 km (5 mi) smaller than longstanding estimates, respectively, along with a margin of error of 0.4 km (0.25 mi) for all estimates. This indicates a 7 percent larger difference between Jupiter’s equatorial radius and its polar radius.
For context, Earth’s equatorial radius is approximately 0.33 larger than its polar radius. These new estimates indicate that Jupiter is approximately 20 times flatter than Earth despite Jupiter being more than 300 times as massive as Earth, also being able to fit more than 1,300 Earths inside it.
“We tracked how the radio signals bend as they pass through Jupiter’s atmosphere, which allowed us to translate this information into detailed maps of Jupiter’s temperature and density, producing the clearest picture yet of the giant planet’s size and shape”, said the study’s co-author, Maria Smirnova, who is a PhD student at the Weizmann Institute of Science and spearheaded the development of a novel method for processing the latest data from Juno.
Despite being slightly slimmer, Jupiter still proudly boasts its massive size and remains the largest planet in the solar system. However, studies like this demonstrate how far methods have improved in just the 50 years since Jupiter was first explored by spacecraft. It also demonstrates how these methods could be employed to other planetary bodies throughout the solar system, including the other gas giants Saturn, Uranus, and Neptune.
What new insight into Jupiter’s physique will researchers make in the coming years and decades? Only time will tell, and this is why we science!
New photos captured by NASA's Curiosity rover show that Mars' giant, spiderweb-like "boxwork" features are covered in tiny, never-before-seen nodules that bear a striking resemblance to arachnid eggs. And researchers are struggling to explain them.
NASA has released two new images of spiderweb-like "boxwork" structures captured by the Curiosity rover on the surface of Mars. One of these photos (encircled) shows tiny, never-before-seen nodules affixed to the surface of these rocky ridges.(Image credit: NASA/JPL-Caltech/MSSS)
NASA's Curiosity rover has snapped stunning new photos of giant "spiderwebs" zig-zagging across the surface of Mars. One of these images has revealed never-before-seen, egg-like spheroids covering the sprawling structures — and scientists are struggling to explain them.
Over the last 8 months, Curiosity has been closely examining a series of interconnected rocky ridges, dubbed "boxwork," on the slopes of Mount Sharp, in the Gale Crater. These ridges, which cover an area up to 12 miles (20 kilometers) across, were created billions of yars ago as ancient Martian groundwater seeped beneath the planet's surface. They were first spotted by orbital spacecraft in 2006, but they have remained largely unexplored until now.
NASA released Curiosity's first boxwork photos in June 2025, shortly after reaching the rocky ridges. But on Monday (Feb. 23), the agency released two more snaps, which showed the structures in much greater detail.
One of these photos, captured Sept. 26 last year, shows off a ground-level view of the ridges, which stand 3 to 6 feet (1 to 2 meters) above Mars' surface. But a second close-up image, snapped on Aug. 21, revealed that some of these ridges are covered in tiny irregular-shaped lumps, or nodules, that have not been seen until now.
One of the new photos, captured on Sept. 26, 2025, shows hundreds of tiny egg-like nodules on the surface of one of the boxwork ridges. And scientists are unsure exactly how they formed. (Image credit: NASA/JPL-Caltech/MSSS)
These nodules bear a striking resemblance to mini spheroids on the surface of a mysterious "spider egg" rock, which was discovered in the Jezero Crater by NASA's Perseverance rover last year and has an unknown origin. And researchers are also having a hard time explaining exactly how the tiny boxwork "eggs" formed.
"We can't quite explain yet why the nodules appear where they do," Tina Seeger, a planetary scientist at Rice University in Houston who is leading Curiosity's boxwork investigations, said in a statement. "Maybe the ridges were cemented by minerals first, and later episodes of groundwater left nodules around them," Seeger said. But more work is needed to confirm if this
However, while the nodules and boxwork have an eerily biological appearance, there is no suggestion that they have any direct ties to extraterrestrial life.
Martian spiderwebs
Boxwork is made up of criss-crossing ridges of mineral-rich rocks that litter the surface of Mars. Similar yet smaller structures are found on Earth, predominantly within caves, and form when calcite-rich water flows between rocks that are eventually eroded, much like how stalagmites and stalactites form, according to the National Speleological Society.
From orbit, the Martian boxwork looks like a giant spiderweb spread out across the Red Planet's surface. (Image credit: NASA/JPL-Caltech/University of Arizona)
However, on Mars, the boxwork was shaped by the fierce winds that scour the planet's surface: "The bedrock below these ridges likely formed when groundwater trickling through the rock left behind minerals that accumulated in those cracks and fissures, hardening and becoming cementlike," NASA representatives previously wrote. "Eons of sandblasting by Martian wind wore away the rock but not the minerals, revealing networks of resistant ridges within."
The team is particularly interested in the patch of boxwork on Mount Sharp because it formed in isolation and is surprisingly high up the mountain's slopes, which has implications for the planet's puzzling watery past.
"Seeing boxwork this far up the mountain suggests the groundwater table had to be pretty high," Seeger said. This hints that the water in this area may have "lasted much longer than we thought," she added.
Researchers hope that further investigation will also shed light on the specific conditions that formed these structures and whether they might have been favorable to any potential ancient Martian microbes.
NASA's Curiosity rover has been exploring the boxwork on the slopes of Mount Sharp for at least 8 months. (Image credit: NASA/JPL-Caltech/MSSS)
"These ridges will include minerals that crystallized underground, where it would have been warmer, with salty liquid water flowing through," Kirsten Siebach, a Curiosity mission scientist at Rice University who has also studied the area, previously said. "Early Earth microbes could have survived in a similar environment. That makes this an exciting place to explore."
After all, what our ears perceive as 'sound' is just a pressure wave that passes through a medium, be that medium a solid, liquid or gas, and agitates the molecules within it.
When that pressure wave hits our ears,it causes small hairs and bones within them to vibrate, which sends an electrical signal to the brain that we interpret as sound.
Soundwaves hit our ears, which our brain interprets as sound. Credit: Jun / Getty Images
But in a vacuum, where there are no molecules of liquid, solid or gas to agitate, that can’t happen – so there is no sound.
But when you’re talking about space, the simple, easy answer is seldom entirely correct – and that’s the case here, too.
That’s because space isn’t actually a vacuum at all.
Yes, huge regions of it are, particularly in interstellar and intergalactic space.
But within galaxies and nebulae are huge, swirling clouds of gas and dust, and the molecules within those clouds are just as capable of being agitated and so passing on a pressure wave – ie, sound – as their counterparts here on Earth.
As if to prove the point, in 2022 NASA released a sound recording of a black hole, extrapolated from observational data from the Chandra X-Ray Observatory.
It turns out black holes make a low-pitched warbling sound that sounds (appropriately enough) like something from the soundtrack of a 1950s sci-fi B-movie.
It’s such a low-pitched sound that your ear wouldn’t be able to hear it naturally, so NASA used a process called ‘sonification’ to render it audible.
Gravitational waves and plasma waves (such as the solar wind, the stream of charged particles that’s constantly being emitted by our parent star) also present a medium through which sound is able to travel.
Not loudly enough that you’d be able to hear it were you there, but clearly enough for it to be detected by Earth-based radio telescopes.
So yes, space is mostly silent – but not truly silent.
Artemis 3 Won’t Land Astronauts on the Moon as NASA Shifts Lunar Mission
Artemis 3 Won’t Land Astronauts on the Moon as NASA Shifts Lunar Mission
NASA has canceled the Artemis 3 moon landing, shifting its focus to testing key technologies and aiming for a safer, more reliable return to the Moon in 2028.
NASA has decided to revise its Artemis program, significantly altering its mission architecture and delaying the anticipated Artemis 3 astronaut landing on the Moon. The decision follows concerns over the readiness of key spacecraft components, such as the Human Landing System (HLS), as detailed in a report by NASA’s Aerospace Safety Advisory Panel (ASAP). Space.com reported this groundbreaking update, noting that NASA aims to reduce mission complexity and avoid rushing the process. As a result, the first crewed lunar landing isnow expected with Artemis 4 in 2028, rather than in the originally planned Artemis 3 mission.
NASA’s Shift in Strategy: A Move Toward Simplicity and Safety
NASA’s decision to cancel Artemis 3’s astronaut landing marks a significant turning point for the Artemis program, which was initially designed to return humans to the Moon by the mid-2020s. One of the main reasons for this shift is the need to reduce the complexity of the mission architecture, according to NASA officials.
“We want to reduce complexity to the greatest extent possible,” said Isaacman during a briefing. “We want to accelerate manufacturing, pull in the hardware and increase launch rate, which obviously has a direct safety consideration to it as well.”
This change in approach will help ensure that NASA can meet its goal of returning astronauts to the Moon safely, without compromising mission objectives.
One of the most important aspects of this decision is how it addresses the concerns raised by the ASAP report, which flagged issues related to the readiness of the Human Landing System (HLS) vehicles. These vehicles, which NASA had contracted from private companies like SpaceX and Blue Origin, are not yet ready to safely transport astronauts to the lunar surface. The delays in meeting critical milestones for these spacecraft, particularly SpaceX’s Starship, led to the decision to reevaluate the timeline and mission structure. The upcoming Artemis 3 mission will now focus on testing key technologies in low Earth orbit, setting the stage for a future crewed lunar landing with Artemis 4.
What Does This Mean for Artemis 3 and the Future of Lunar Exploration?
The cancellation of Artemis 3’s planned Moon landing has serious implications for the overall timeline of NASA’s lunar exploration ambitions. As originally envisioned, Artemis 3 was meant to be the first mission in the program to land astronauts on the Moon since Apollo 17 in 1972. However, NASA’s new strategy aims to take a more cautious, measured approach to ensure that the technology and hardware are fully ready before they are used in a high-stakes mission. In a briefing with Space.com, Isaacman expressed his confidence that this approach is aligned with the recommendations from the ASAP report:
“I think what we’re doing is directly in line with what ASAP asked us to do,” he said. “I think it should be incredibly obvious you don’t go from one uncrewed launch of Orion and SLS, wait three years, go around the moon, wait three years and land on it.”
By emphasizing incremental testing and readiness, NASA hopes to avoid the pitfalls that could undermine a mission of this magnitude.
The new timeline, now targeting Artemis 4 for the first crewed landing in 2028, reflects NASA’s focus on thorough preparation rather than rushing through steps. This delay, while disappointing for some, could ultimately lead to a safer, more successful return to the lunar surface. NASA’s decision underscores the need to ensure that the various components of the mission, including the Space Launch System (SLS) rocket and Orion spacecraft, work seamlessly together. With these changes, NASA hopes to replicate the success of previous space programs by increasing the launch cadence and gaining more experience before landing astronauts on the Moon again.
NASA Faces Delays: Technical Challenges and Solutions
Despite the setback in the Artemis 3 timeline, NASA remains committed to achieving its lunar exploration goals. The agency continues to make progress on the necessary hardware, including the Space Launch System (SLS) and Orion spacecraft, which are being tested in preparation for Artemis 2. However, there have been significant delays and challenges, particularly with the SLS rocket. During a recent briefing, Lori Glaze, NASA’s acting associate administrator for the Exploration Systems Development Mission Directorate, addressed an issue with the rocket’s helium flow system:
“The suspected system component for the helium flow will be removed, and they’re going to undergo detailed sections and assess the cause of the issue,” she said. “We hope to get down to the root cause of that and make changes, not just to the hardware, but to our operational procedures, so that we don’t encounter the same issue again when we roll back out to the pad.”
This technical difficulty, along with other challenges faced in the development of the HLS vehicles, underscores the complex nature of space exploration. While the delay is frustrating, it also provides an opportunity to make adjustments and learn from past mistakes to ensure that future missions are not hindered by avoidable issues.
NASA’s Perseverance Rover Caught Crackling Sounds on Mars. Researchers Think It Was Electricity
NASA’s Perseverance Rover Caught Crackling Sounds on Mars. Researchers Think It Was Electricity
Two separate NASA missions detected unusual signals on Mars, a strange sound on the surface and a rare reading from orbit, and scientists are still trying to understand what they mean.
Two NASA spacecraft have detected different signals that point to possible lightning on Mars. One clue comes from orbit, the other from the planet’s surface, together strengthening the case that electrical discharges flicker through the Red Planet’s dusty skies.
Lightning has already been observed on Jupiter, Saturn, and Neptune. Mars, by contrast, has remained ambiguous territory. Its atmosphere is thin, and its magnetic field exists only in small, scattered patches, conditions that make any lightning harder to detect and likely very different from the bright bolts seen on Earth.
Scientists have long hypothesized that if lightning occurs on Mars, it would resemble faint electrical sparks generated by swirling, electrostatically charged dust. Now, recent findings based on data from NASA’s MAVEN orbiter and the Perseverance rover suggest those sparks may indeed be real.
A Rare Radio “Whistler” Detected by MAVEN
The most recent evidence comes from a study published on February 27 in Science Advances. According to the research, scientists identified a possible lightning signature in data collected in June 2015 by NASA’s Mars atmosphere and volatile evolution (MAVEN) spacecraft.
Schematic representation of the conditions and processes that produce a whistler signal.
Credit: Science Advances
The team, led by Ondřej Santolíkof the Czech Academy of Sciences, searched for radio signals known as “whistlers.” When lightning strikes, it heats and ionizes surrounding air, allowing radio waves to travel through the atmosphere and into space. On a receiver, these waves produce a characteristic whistle-like tone. Researchers reviewed 108,418 data snapshots from MAVEN. Santolík explained that:
“That needs to be done visually because it’s very hard to do it by a machine because of the noise features in the data”. Out of that extensive dataset, the team identified only one candidate signal. “It’s very surprising that we found it at all.”
The scientists then spent a year confirming that the signal matched what would be expected from lightning. NASA has reportedly been out of contact with MAVEN for nearly three months, leaving open questions about whether similar observations will be obtained in the near future.
Perseverance Hears Crackling During Dust Storms
A few months earlier, a separate group of researchers presented another form of evidence based on recordings from a microphone aboard NASA’s Perseverance rover.
The team identified dozens of crackling sounds produced by small electrical discharges during dust storms near the rover. These sounds likely reflect localized electrical activity within charged dust clouds rather than large-scale lightning bolts.
Spectrogram showing the frequency evolution of electromagnetic waves detected by MAVEN.
Credit: Science Advances
Karen Aplin, a space physicist at the University of Bristol who was not involved in either study, said the two findings together give “a feeling that we’re closing in on Mars lightning.” She noted that on Earth, different types of electrical discharges exist, ranging from thunderstorm lightning to the glow known as Saint Elmo’s fire, suggesting that Mars could host varied electrical phenomena as well.
A Discovery With Bigger Implications Than It Seems
Electrical discharges also influence atmospheric chemistry. As reported by Scientific American, lightning has been shown to spark chemical reactions that may contribute to the development of life. Understanding whether similar processes occur on the Red planet could help scientists interpret the planet’s chemical environment.
For Santolík, the findings are bittersweet. He was part of a team that developed a dedicated lightning detector for the Russian-made lander of the Rosalind Franklin rover, part of the European Space Agency (ESA) program. The mission, initially planned for 2022, was disrupted after Russia’s full-scale invasion of Ukraine.
ESA is now building its own lander for a 2028 launch but chose not to include instruments on the platform to speed construction. The lightning detector has since been returned to its creators and is not expected to fly to Mars.
At this stage, asingle orbital “whistler”andcrackling sounds detectedat the surface stand as the strongest hints yet that the Red Planet may host elusive, dust-driven sparks in its skies.7
Researchers have identified powerful Martianelectrical discharges, similar tolightning, and strong enough to be observed from orbit, in new research bringing this extraterrestrial phenomenon to light.
Mars and Earth feature very different environments—namely, the Red Planet lacks a global magnetic field and possesses only a thin atmosphere. As a result, lightning does not form in rain clouds as it does on Earth; instead, intense activity in dust storms and dust devils produces the electrical charge that generates Mars’ lightning-like electrical discharges.
MAVEN Observes Martian Lightning
NASA’s MAVEN orbiter made the crucial observation a decade ago, but only in December 2024 did the significance of the signals become clear. Recently, Czech researchers completed their analysis and revealed the findings in a new paper published in Science Advances.
“I went through data from the beginning of the mission, and after automatically filtering records measured outside areas of strong magnetic fields or at excessively high altitudes,” František Němec of Charles University said in a press release. “I found only a single electromagnetic lightning signal—a so-called whistler—among thousands of possible records.”
“Based on previous calculations, laboratory experiments, and observations of lightning in the dust plumes of terrestrial volcanoes, we all expected electrical discharges in the Martian atmosphere, but until that moment, no one had recorded them,” said Ondřej Santolík of the Czech Academy of Sciences and Charles University.
MAVEN—short for Mars Atmosphere and Volatile Evolution—was designed to study the Martian atmosphere and its evolution. Operating from 2014 until NASA lost contact in December 2025, the spacecraft examined interactions between the solar wind and the atmosphere. To support this mission, it carried instruments capable of measuring electromagnetic waves, which ultimately detected the lightning signal.
A Lucky Observation
Observing the lightning-like discharge required unusually precise circumstances. The MAVEN orbiter had to be at the correct altitude and position, and in the proper observation mode, at the moment the event occurred. Conditions on Mars also had to allow the signal to escape into space. Without a global magnetic field, lightning appears to form only in regions with localized fields, and for detection, those fields must be both strong and largely vertical. The signal also had to reach the ionosphere without losing strength.
Later observations by the Perseverance rover in 2021 and 2024 detected lightning-like discharges as well, though the researchers believe those represent a different phenomenon.
“In the thin atmosphere of Mars, the accumulation of large potential differences is limited by the onset of small, local glow discharges. Such discharges may be those detected by Perseverance,” Němec told The Debrief. “However, they are too weak and too localized to be detected by an orbiter.”
“A discharge detectable from orbit would have to be significantly stronger, involving a larger potential difference distributed over comparatively large spatial scales,” Němec added. “This most likely indicates that the mechanism responsible for generating the corresponding voltage must be different.”
The Lightning of Mars
Martian lightning discharges produce a cascading effect. A short, powerful current generates fluctuating magnetic and electric fields that propagate outward as electromagnetic waves. When part of the wave reaches the ionosphere, it slows, and different frequencies travel at different speeds, arriving at the orbiter separately. Higher frequencies travel faster and reach MAVEN first.
PhD student Kateřina Rosická developed a simulation to test this hypothesis, combining a model of Earth with the assumed composition of the Martian ionosphere. The simulation showed that lower-frequency waves would be delayed while higher-frequency waves would attenuate—exactly what MAVEN observed. The spacecraft’s failure to detect higher frequencies matched the prediction.
Whether the phenomenon strictly qualifies as “lightning” remains uncertain. For now, researchers describe it as a lightning-like electrical discharge.
“The common understanding is that the phenomenon of lightning encompasses various related effects, such as a visible flash,” Němec explained. “Of all these effects, the available measurements allow us to demonstrate only the sudden release of low-frequency electromagnetic radiation.”
“In other words, there is nothing yet that clearly separates this phenomenon from lightning, but the available instrumentation does not allow us to observe all the effects that the common understanding of lightning encompasses,” Němec added. “We therefore cannot confirm or exclude them, and it is possible that in the thin atmosphere of Mars some of these effects may differ significantly from those known on Earth.”
Keeping an Eye On Mars Lightning
For now, the researchers say the phenomenon poses little threat to future crewed missions.
“Based on observations on Earth, lightning is generally not particularly deadly or dangerous, at least when reasonable precautions are taken,” Němec said. “It could, for example, endanger surface antenna equipment by destroying its electronics; however, I would say it is not too significant a concern.”
Currently, the European Space Agency (ESA) is considering an unscrewed Mars mission called M-MATISSE for a possible 2037 launch, which the team says would provide vital new information on any Mars lightning-like electrical discharges.
“It will be better equipped to search for traces of lightning discharges than its predecessor, MAVEN,” said study co-author Ivana Kolmašová, who also serves as a member of the ESA Scientific Study Team for the M-MATISSE mission. ESA is expected to decide by the end of this year whether it will pursue the mission.
Ryan Whalen covers science and technology for The Debrief. He holds an MA in History and a Master of Library and Information Science with a certificate in Data Science. He can be contacted at ryan@thedebrief.org, and follow him on Twitter @mdntwvlf.
New Discoveries on Mars and What They Say About Habitability and Life
New Discoveries on Mars and What They Say About Habitability and Life
By Nathalie A. Cabrol, Astrobiologist & Science Director, Carl Sagan Center, SETI Institute.
Gale crater: These pea-sized nodules were formed by minerals left behind as groundwater was drying out on Mars billions of years ago.
(Credit: NASA/JPL-Caltech/MSSS)
At a Glance:
New Discoveries on Mars and What They Say About Habitability and Life Nathalie A. Cabrol, SETI Institute
Two NASA rovers have strengthened the case that ancient Mars may have supported life.
Curiosity (Gale Crater)detected the largest organic molecules yet found on Mars—long carbon chains consistent with fragments of fatty acids.
These moleculeswere preserved in rocks altered by ancient groundwater, suggesting long-lived subsurface water activity.
Perseverance (Jezero Crater) identified silica-rich rocks, including quartz, minerals known on Earth for preserving biosignatures.
The rover also found kaolinite clay, evidence of sustained water–rock interaction and potentially habitable conditions.
Why it matters: While not evidence of life, these discoveries show that ancient Mars had complex organic chemistry, long-lasting water systems, and mineral environments capable of preserving potential signs of life—making the search more compelling and increasingly testable.
Mars dominates the planetary news with exciting reports. Two NASA rovers, working nearly 3,700 kilometers apart, made discoveries that addressed the question: how far did Mars come toward conditions that, on Earth, supported life?
On one side of the planet, new studies confirm last summer’s hint that Curiosity detected the largest organic molecules yet identified on Mars. These include decane, undecane, and dodecane found in the ancient Cumberland mudstone of Gale Crater. These C10–C12 carbon chains are consistent with the kinds of fragments you might expect from fatty acids, which are molecules that, on Earth, sit close to biology because they are basic building blocks of membranes and metabolic chemistry. But it now seems that these compounds were in sediments later modified by groundwater-driven diagenesis (when sediments turn into rocks), documented by Curiosity’s mineralogical and geochemical measurements. On the other side, Perseverance has identified silica-rich rocks in Jezero Crater, including opal/chalcedony and, critically, well-crystallized quartz, detected with SuperCam spectroscopy. Why does it matter? Silica-rich phases on Earth are famously good at preserving biosignatures, from molecular residues to microtextures. And we just learned that Perseverance also identified kaolinite in altered igneous rocks on the crater floor. This comes from combined SuperCam infrared spectroscopy and PIXL elemental chemistry, consistent with a feldspar-to-kaolinite transformation under sustained water activity. If both findings are mineralogical firsts, they are also a lot more than that. They point to abundant ancient groundwater–rock interaction and likely hydrothermal processes.
Taken together, these are not “We discovered life on Mars” headlines. They are subtler and, in many ways, more important. This is a strengthening of the case that ancient Mars had both (i) an organic carbon inventory and (ii) environments capable of concentrating, processing, and preserving chemical traces – and these environments were diverse and long-lasting, and that’s good news for the search for life on Mars.
Organic Molecules and Ancient Groundwater at Gale
The findings at Gale are exciting because they push Martian organic chemistry into a higher tier of complexity. Long carbon chains do not automatically mean biology, but they do mean that Mars can make, or at least retain, molecules that are closer to the chemical scaffolding of life than the simple organics we often discuss. On Earth, fatty acids are associated with life, but they are not exclusive to it. Abiotic pathways exist, including hydrothermal synthesis and Fischer–Tropsch-type reactions (chemical reactions on hot mineral surfaces that can build organic molecules capable of supporting life). Mars has the rocks, the heat sources (past and still some today), the CO/CO₂ and H₂ chemistry, and time, lots of it.
What now makes the Cumberlands organics particularly compelling is their geological context. Curiosity has shown that these mudstones underwent multiple episodes of groundwater circulation after burial. These episodes have been recorded in mineral veins, diagenetic textures, and chemical redistribution measured by CheMin and APXS. The organics detected by SAM therefore reside in rocks that remained chemically open systems for extended periods. That matters a lot because groundwater does more than wet rocks. It transports carbon, redistributes redox couples (paired chemicals that exchange electrons), and creates microenvironments where organic molecules can be synthesized, altered, concentrated, or shielded from oxidation. Subsurface aqueous systems are also among the most stable habitable niches on Earth, persisting long after surface environments become hostile. In Gale, this implies that potential habitable conditions did not end with the lake that deposited the mudstone but continued underground, in circulating water, for geologically meaningful timescales.
What nudged this discovery into deeper interest is not the mere detection of the molecules, but the attempt to ask whether known non-biological sources plausibly account for their abundance. A follow-on analysis reported by NASA describes a study arguing that the non-biological sources they evaluated (for example, delivery by meteorites) could not fully explain the measured abundance, making it “reasonable to hypothesize” that biology could have contributed, while stressing that this remains unresolved.
Jezero: Hot Springs, Clay, and Life-Friendly Environments
The Jezero quartz story is exciting for different reasons. It is less about “life ingredients” and more about environmental opportunity. Quartz and its silica cousins (opal, chalcedony) typically form under conditions that mobilize silica in water and precipitate it, often in hydrothermal settings. The Jezero detections are interpreted as part of a common hydrothermal system, potentially triggered by the impact that formed Jezero, with different silica phases representing precipitation at different depths and temperatures. Why does that matter with respect to habitability? Because hydrothermal systems are among the most compelling natural laboratories for prebiotic chemistry and microbial ecosystems. They supply heat, chemical gradients, and mineral surfaces that can drive synthesis and catalysis. And if life ever gained a foothold, hydrothermal circulation can both sustain it and entomb its traces. Silica-rich deposits are also preservation jackpots. On Earth, cherts and other siliceous rocks can lock away molecular organics and microscopic structures over immense timescales. The Jezero team explicitly frames these silica-rich rocks, especially opaline silica, as key targets for sampling and return, precisely because of their preservation potential.
That, in itself, is already a tremendous finding, but there is more. The identification of kaolinite announced a few days ago now expands the picture from hydrothermal pulses to prolonged water alteration. Kaolinite typically forms when feldspar-rich igneous rocks interact with liquid water over extended periods under relatively moderate temperatures and pH conditions. Its presence in Jezero’s altered crust indicates sustained water-rock interaction. Critically, Perseverance observes kaolinite spatially associated with silica-bearing alteration zones. Together, these minerals outline a continuum of water environments, from hydrothermal circulation to longer-lived alteration in percolating or standing waters. This kind of mineralogical diversity is exactly what on Earth correlates with habitable geochemical gradients and long-term fluid activity.
NASA's Perseverance rover discovers bleached kaolinite rocks on Mars, revealing clues of ancient climate conditions in Jezero Crater.
What Makes a Biosignature?
Here is the key: neither discovery stands alone. Organic molecules, by themselves, are not proof of life. Quartz, by itself, is not proof of life. Even both together are not proof of life. But they add weight to an accumulating argument that ancient Mars wasn’t merely “wet once,” or “chemically interesting in theory.” It was active, carbon cycling through environments, water moving through rocks, hydrothermal systems likely operating, and complex organics being produced, delivered, preserved, or all the above. The addition of groundwater-altered sediments at Gale and clay-forming alteration at Jezero further suggests that habitable conditions were not confined to short-lived surface lakes or impact events but extended into subsurface and long-duration aqueous systems across different regions of the planet. This is why astrobiology relies so heavily on context and the ladder of life-detection principles. The same molecule means different things in different rocks. The same mineral means different things in different settings. A signature of life is convincing only when it cannot be explained by the environment alone. What is not helping either is that we still do not have a universal definition of life that can be cleanly adopted for alien worlds. We recognize life on Earth because Earth is saturated with it and because we understand its biochemistry here. On Mars, we are forced to adopt a more cautious approach, inferring possibilities and building confidence only when multiple independent clues converge.
The Significance of these Discoveries
Gale’s organics grow the chemical inventory. Gale’s groundwater history and Jezero’s kaolinite now extend both inventories in time and environmental range, indicating that water activity and alteration persisted beyond the initial lake and impact phases, and occurred in multiple geochemical regimes. Together, they help narrow the space of plausible histories for Mars, histories in which complex carbon chemistry had time and place to unfold, and in which traces of life, if they ever existed, might still be readable. Ancient Mars, increasingly, looks less like a planet that was briefly habitable and more like one that sustained habitable settings in different places, at different depths, and for much longer than once thought. These findings do not tell us that life was present on Mars, but they tell us the question remains scientifically… alive and increasingly testable. And in Mars exploration, that is a very big deal.
What NASA’s Newest Discovery On Mars Means Mars has always been our neighbor in the universe but remained distant enough to remain a secret. Whenever NASA releases a new finding, people are curious once again. The latest findings about the Red Planet are not an exception. Although the details are still under research by scientists, there are good indications that there is something that could alter the way we mentally process Mars and its past in a rather gentle way. It does not suggest any dramatic conclusions or immediate answers. Rather, it initiates a philosophical debate on the possibility, the patience, and the gradual yet constant manner in which science proceeds. And that perhaps could be the most interesting of all.
A closer look at the Martian surface New information seems to point out strange surface patterns not evidently perceived previously. These structures might have been formed in the course of time. Although the researchers are cautious, the shapes and textures may provide some new information regarding the changes in the environment on Mars.
Hints of ancient water activity According to some experts, the new findings may be related to evidence of the movement of water in the past. In the event that that happens to be the case, it may support previous theories that Mars was once in wetter conditions. Nonetheless, it will take a greater analysis and time to be validated.
What the soil samples could reveal The samples of the soil collected can have traces of chemicals that assist the scientists in knowing the past of the planet. Minute combinations of minerals could indicate certain ecological factors. Nevertheless, the interpretation of these signals is complicated and not always easy.
Technology is making it possible This discovery has been made possible by advanced instruments on rovers and orbiters. These instruments are meant to screen finer details that could have been overlooked by the older missions. All the reading, however, should be carefully checked.
The role of rover exploration Missionary vehicles such as the Perseverance rover are still relaying useful information. They have mobility and are able to learn various terrains. The recent developments could be a component of the ongoing research on the selectively chosen areas.
Why location matters on Mars What is discovered might not be any more important than the location of the discovery. Some areas are more historical about geology than others. Scientists tend to concentrate on the locations that could have been water-bearing in the past.
The question of past life Life is always something that people are inquiring about whenever Mars unveils something new. Although this finding does not validate anything, it could be used to provide background for the bigger search. Researchers are rather slow in addressing such possibilities.
Learning the history of martian climate Climate significantly contributes to the formation of any planet. The new information may give an indication of the way Mars evolved millions of years ago. It may imply changes in temperature or atmosphere, but further studies are required.
Why scientists avoid quick conclusions Scientific findings do not often give immediate solutions. Any discovery has to be put to the test, scrutiny, and argument. This cautious approach prevents confusion. The latest find on Mars is bound to take the same deliberate direction
Interstellar comet 3I/ATLAS is soon to have a potentially course-altering encounter, before it heads out of our Solar System for good in the direction of the Gemini constellation.
Last year, the Solar System received its third confirmed interstellar object, in the form of interstellar comet 3I/ATLAS. This comet has traversed the galaxy for billions of years, and is likely older than the Solar System it is currently passing through.
The object has already had its closest encounters with Mars, Earth, and the Sun. The encounter with the Sun saw 3I/ATLAS change dramatically, with a massive release of organic molecules, while the approaches to Earth and Mars weren't close enough to have a large effect on the comet.
The Sun Just Cracked Open 3I/ATLAS Revealing New Surprises
But before our interstellar visitor leaves us for good, it has one last close encounter to go, and it's possible it might be a course-altering close shave. On March 16, the object's path will take it close to our largest gas giant. On that day, it will pass within 0.35832 astronomical units (AU) of Jupiter, with one AU being the average distance between Earth and the Sun.
Why is that significant? It is incredibly close to Jupiter's "Hill radius" or "Hill sphere". This is the region around a massive body where its gravity dominates over more distant objects like the Sun. Jupiter's Hill radius is around 0.355 AU, or around 53 million kilometers (33 million miles).
"The comet 3I will definitely suffer the perturbation from both Mars and Jupiter at their respective close approach epochs," the authors of one preprint study (a paper that has yet to be peer-reviewed), which used dynamic simulations to map 3I/ATLAS's path, explained ahead of the close encounter with Mars.
"The effect of Jupiter will be larger due to the fact that the comet is passing very close to the Hill radius of Jupiter," the team wrote.
Whether this encounter will significantly affect the course of 3I/ATLAS, however, depends on the non-gravitational acceleration of the object. Though this sounds kind of spaceshippy, all it means is the acceleration that isn't due to gravitational interactions alone, but factors such as outgassing and radiation pressure from the Sun.
"We find that the major effects on comet 3I’s orbit are seen when the nongravitational acceleration is of the order of 10 to 10 auday," the authors explained. "The non-gravitational acceleration of 10 auday and lower has negligible effect on the various parameters."
Mapping the comet's path back and forward over longer timescales, the team found that it likely came from the direction of the Sagittarius constellation, and it will depart in the direction of Gemini. Before that, we will have another opportunity to study the object as it approaches Jupiter. So long, very old friend.
It’s like something out of a Hollywood blockbuster: an astronaut looks out the window and suddenly notices a thin crack running across the glass, separating him from the deadly vacuum by just a few centimeters. But what happened to the crew of the Chinese Shenzhou-20 missionlast November was not a movie, but a harsh reality that nearly led to a catastrophe in orbit.
The Shenzhou-21 spacecraft capsule with the Shenzhou-20 crew at the landing site in the Inner Mongolia Autonomous Region in northern China on November 14, 2025. Source: Xinhua
Commander Chen Dong was the first to notice the danger. What at first appeared to him to be ordinary trash or a leaf stuck to the glass turned out to be much more sinister. A triangular mark was clearly visible on the inner surface of the window — a crack left by a collision with an unknown object.
“I went out to inspect it, and my eye immediately noticed this anomaly,” recalled the commander. In an instant, realization came with a chill of fear: their station had been attacked by a piece of space debris. Scientists still do not know its origin, but they assume that the deadly guest was no larger than a millimeter. This proved sufficient to break through the spacecraft’s strong defenses.
Don’t panic
Despite the dramatic nature of the situation, there was no panic on board. Taikonaut Wang Jie, who was responsible for safety, handled the incident with professional calm. He explained that the design of the porthole was not just simple glass, but a complex engineering system.
“The outer layer is just a protective screen, a kind of ‘shield’. The main pressure is held by two inner sealed layers,” he reassured the audience. For detailed analysis, the astronauts used a special microscope that looked like a pen. They were shocked by what they saw: a network of cracks, some relatively long, others shorter, but the most dangerous thing was that some of them went right through the material.
Rescue operation
Unlike in movies, where everything is decided in seconds, the real drama unfolded over several days. However, the consequences could have been catastrophic. The damaged Shenzhou-20 could no longer be used to return the crew home. The risk of depressurization during descent was too great.
The Chinese flight control center quickly developed a rescue plan. The crew of Shenzhou-20 was forced to abandon their spacecraft and temporarily “move” to the station. They returned home in the Shenzhou-21 capsule, which was originally intended for their replacements. This created a new problem: the new crew was left in orbit without a vehicle.
The situation was saved by the fact that the empty emergency Shenzhou-20 was later successfully undocked and returned to Earth in automatic mode.
Warning for the future
Photos of collisions show how destructive even minor impacts on a spacecraft’s hull can be. Photo: NASA
This incident is not just a story about successfully avoiding disaster. This is a stern warning to all those who are exploring near-Earth space today. Our orbit has turned into a crowded garbage dump, where thousands of objects are hurtling around at breakneck speed.
We will never know what exactly hit Shenzhou-20 — a microscopic fragment of an old rocket or paint from another satellite. But scientists unanimously warn that a chain reaction of collisions (Kessler syndrome) could render space unsuitable for flights for decades.
In early January, NASA unexpectedly announced it had been forced to delay a scheduled spacewalk involving two crewmates on board the International Space Station, citing a “medical situation” that “involved a single crew member who is stable.”
Two days later, the agency announced the first-ever medical evacuation in the space station’s 25 years of continuous human occupation, a historic moment highlighting the possible severity of the situation.
The affected crew members of the Crew-11 mission — NASA astronauts Mike Fincke and Zena Cardman, Japanese astronaut Kimiya Yui, and Russian cosmonaut Oleg Platonov — safely splashed down in the Pacific Ocean off the coast of southern California on January 15 and were promptly helicoptered to the nearby Scripps Memorial Hospital La Jolla near San Diego, leaving us with far more questions than answers.
Now, seven weeks later, Fincke has voluntarily stepped forward, announcing in a NASA statement that it was he who had “experienced a medical event that required immediate attention from my incredible crewmates.”
Fincke is a retired US Air Force colonel and was selected to be an astronaut back in 1996. The Crew-11 mission, which launched in August, was his fourth trip to space. He was also initially selected in 2019 to pilot Boeing’s much-troubled Starliner spacecraft, but — perhaps fortunately — never got the chance.
“Thanks to their quick response and the guidance of our NASA flight surgeons, my status quickly stabilized,” Fincke said. “I am deeply grateful to my fellow Expedition 74 members… as well as the entire NASA team, SpaceX, and the medical professionals at Scripps Memorial Hospital La Jolla near San Diego.”
But beyond revealing a “carefully coordinated plan to be able to take advantage of advanced medical imaging not available on the space station,” we still don’t know what caused the space station’s first medical evacuation in history, leaving us with the simple question: why come forward without revealing what happened?
In a statement to Futurism, NASA press secretary Bethany Stevens said it was Fincke’s choice to identify himself as the crew member who had the medical incident, not NASA.
“Given medical privacy laws and the overall sensitivity of the situation, this decision was entirely up to the individual involved,” Stevens wrote. “We know now, that in this case, that was Mike Fincke, because he self-identified.”
Stevens also suggested that Fincke may have chosen to protect his fellow crew members from being the subject of speculation and unfounded conspiracy theories.
“I can’t speak to Mike’s motivations in self-identifying, but given the scrutiny and speculation, I would guess he is hopeful that his brave step forward will decrease the conspiracies online that target his crewmates,” Stevens added in her statement to Futurism.
Needless to say, it’s a delicate matter. Fincke could have a litany of personal reasons not to publicize any details regarding his earlier condition that required an evacuation, and he’s entirely within his rights to withhold that information.
But given the extremely public nature of his employment as a NASA astronaut, questions are bound to arise, especially given it’s the first-ever medical evacuation of its kind.
It’s ultimately up to Fincke to tell the likely harrowing tale. But when or if that will happen remains unclear.
K2-18b is a so-called Habitable Zone planet located 124 light-years away from us. In terms of mass, the planet is somewhere between Earth and a small gas giant. Researchers are interested in whether extraterrestrial life could exist on it.
If you have been following exoplanet research over the past few years, you have probably heard of K2-18b. Located 124 light-years away in the constellation Leo, it has attracted a lot of attention because it is right in the habitable zone of its red dwarf star, and measurements from the James Webb Space Telescope show that its atmosphere is rich in carbon dioxide and methane. It is one of the leading candidates for the title of “hydrogen world” — a world where a dense atmosphere rich in hydrogen covers a global ocean of liquid water.
This is such an interesting target for researchers from the Search for Extraterrestrial Intelligence (SETI) project that they have directed two of the world’s most powerful radio telescopes to observe the K2-18b system. A recent article available on the arXiv preprint server shows that, despite millions of potential matches, this planet is unlikely to be sending out artificial narrowband radio signals equivalent to our level of technology.
Listening with radio telescopes
To collect the data needed for processing, both the Karl G. Jansky Very Large Array (VLA) in New Mexico and the MeerKAT radio telescope in South Africa were used. These are the two most powerful radio telescopes on the planet, and their coordination within the observation campaign is an extremely rare occurrence.
But physical equipment was not the only important factor for this work. The “data transfer channel,” as astronomers call the software filters and logic applied after data collection, is no less important, especially in radio astronomy. Signals from Earth are the source of the vast majority of radio signals received by these telescopes, and modern filtering algorithms, such as the Commensal Open-Source Multi-Mode Interferometer Cluster system used by the VLA, and the Breakthrough Listen User Supplied Equipment (BLUSE) system used by MeerKAT, are important elements of any modern radio astronomy program.
Radio signal filtering system
However, the logic behind such filtering remains the responsibility of the people involved in the process, and the article describes five different restrictions they impose on the data for selecting potential alien technosignatures. The first step was to mask radio frequency interference — essentially, they removed all data from signals falling within frequency ranges known to be heavily contaminated by terrestrial interference. If aliens communicated through these channels, we would have to use some other method — such as a radio telescope on the far side of the Moon — to hear them.
Doppler effects, such as the changing sound of an ambulance siren as it approaches or passes you, are even more noticeable when the signal travels between planets. Any signal with virtually no Doppler effect was immediately rejected, as it could only have originated from Earth. Perhaps the most controversial logical filtering choice was to exclude all signals with a signal-to-noise ratio of less than 10 or greater than 100. Although this allowed for the exclusion of extremely weak false positives, as well as strong instrumental data artifacts typically observed in only one antenna, it could also exclude.
Another filtering technique is the use of multi-beam analysis. In this case, the telescopes formed coherent beams across the sky, one of which was directed directly at K2-18b, and the other at a different location. In such cases, the signal coming from the exoplanet would only appear in the beam directed directly at it, while terrestrial interference penetrates several beams simultaneously. The final check, which was not necessary due to the timing of the study, is transit filtering. Any signal coming from K2-18b should disappear when the planet passes in front of its parent star, but since no such “secondary transit” occurred during the observation, filtering was not necessary.
Positive test result in any case
In short, despite millions of potential signals throughout the observation period, none of them passed these filters. No unambiguous technosignatures were detected in the narrowband radio spectrum from K2-18b. Although this may seem disappointing, it is precisely this kind of thing that science needs in order to progress. By carefully scanning the planet and finding nothing, they can establish the “upper limits” of the transmitter’s power from this system — in terms of power, it would be equivalent to the destroyed Arecibo radar in Puerto Rico. If there is civilization there, it certainly does not scream at us from anything greater than this level of radio telescope.
However, perhaps the most important result is the confirmation of the concept of their automated filtering system. Processing millions of signals detected by two telescopes manually would be virtually impossible. So, when even larger radio telescopes such as the Square Kilometer Array appear, these technologies will be ready to help other research projects make sense of the mass of data collected. Although planet K2-18b may be quiet today, we will continue to improve our ability to listen if it ever begins to communicate with us.
On the night of February 24-25, US PresidentDonald Trump made history by giving the longest speech on the state of the nation — it lasted 107 minutes. The main topics were economic successes, criticism of the Democrats, and the fight against illegal immigration. However, amid the political statements, an event worthy of special attention has been overlooked: the country is preparing to send a human into deep space for the first time since the legendary Apollo program.
Artemis II astronauts (left to right): Canadian Space Agency mission specialist Jeremy Hansen, pilot Victor Glover, commander Reid Wiseman, and mission specialist Christina Koch attend the President’s address to Congress during a joint session of Congress at the U.S. Capitol on February 24, 2026. Photo: Gizmodo
The most ironic thing is that the main characters of the upcoming space breakthrough went unnoticed, even though they were sitting in the front row. The astronauts of the Artemis II mission— Reid Wiseman, Victor Glover, Christina Koch from NASA, and Jeremy Hansen from the Canadian Space Agency — were guests of honor of the Speaker of the House of Representatives. These four brave souls are about to embark on a journey to the Moon that no human being has undertaken in more than fifty years.
Their 10-day flight will be more than just a symbolic gesture. This will be the farthest human expedition in the history of space exploration, taking the Orion spacecraft into orbit around our natural satellite.
The Trump administration’s vision
The Artemis II mission is intended to lay the foundation for a “golden age of American space leadership” — a phrase that the Trump administration uses quite often. However, the president limited himself to brief references to Apollo’s glorious past and boastful statements about the creation of the US Space Force, proudly calling it “his brainchild.”
However, the significance of Artemis II extends far beyond political ambitions. This is a critically important test phase: for the first time, the super-heavy Space Launch System (SLS) rocket and the Orion spacecraft will be tested with a crew on board. The success of the mission should confirm the US’s ability not only to return to the Moon, but also to make long-term plans for expeditions to Mars.
Space race gains momentum
The importance of the program is reinforced by the international context. China is actively developing its own manned lunar program, adding an element of healthy competition and urgency to American efforts. Maintaining NASA’s technological supremacy is not only a matter of prestige, but also of national security and scientific leadership.
However, despite its historical context and geopolitical significance, the mission faces an unexpected enemy — public indifference. Even among space enthusiasts, interest is beginning to wane due to technical problems. It was recently announced that SLS and Orion are returning to the hangar, postponing the likely launch until at least April.
A missed opportunity to unite the nation
The problem of lack of attention is not just a matter of NASA’s “public relations.” Without broad public support, multi-billion-dollar space programs become vulnerable targets for budget cuts. Trump had a unique opportunity to draw the attention of a 300 million-strong audience to the titanic feat that his compatriots are preparing to accomplish for the first time in half a century. He could present the astronauts sitting in the hall and explain the significance of their mission for the future of humanity.
Instead, time was spent on political tirades. By failing to seize this opportunity, the president did more than simply ignore an important event — he dealt a blow to his own space policy, depriving it of potential public support at a time when it needs it most.
JWST observed Uranus for nearly a full rotation, charting the planet's upper atmosphere and magnetic environment for the first time.
JWST observed Uranus rotating for 15 hours in January 2025, showing bright auroral bands (in white) near the planet's magnetic poles.
(Image credit: ESA/Webb, NASA, CSA, STScI, P. Tiranti, H. Melin, M. Zamani (ESA/Webb))
Scientists using the James Webb Space Telescope just mapped the mysterious upper atmosphere of Uranus for the first time, revealing strange new features of the planet's mysterious magnetic field and glowing auroras.
The James Webb Space Telescope (JWST) observed Uranus rotating for 15 hours (nearly a full Uranian day) to learn more about how ice giants distribute energy in the upper layers of their atmospheres and to investigate how the planet's auroras operate.
To learn more, scientists used JWST to study Uranus' magnetosphere — the region of space around Uranus that's dominated by the planet's magnetic field.
"Uranus's magnetosphere is one of the strangest in the solar system," study lead author Paola Tiranti, a doctoral student at Northumbria University in the U.K., said in a European Space Agency (ESA) statement. "Webb has now shown us how deeply those effects reach into the atmosphere."
Strange lights on Uranus
JWST charted "the most detailed portrait yet" of how particles in Uranus' upper atmosphere are energized (ionized) by interactions with the sun, ESA officials said in the statement. The study, published Feb. 19 in the journal Geophysical Research Letters, aimed to measure ion temperature and density as far as 3,100 miles (5,000 kilometers) above the cloud tops of Uranus.
Temperature and density do not peak at the same altitude, JWST showed. Ions were the warmest between roughly 2,500 and 3,100 miles (4,000 and 5,000 km) but the densest at about 600 miles (1,000 km). This is because of the "complex geometry" of the planet's magnetic field, ESA officials said in the statement.
That geometry also produced two bright bands of auroras near Uranus' magnetic poles. In between the aurora belts, however, there is a "depletion" in both ion density and auroral emissions — an effect likely produced by transitions between the planet's magnetic-field lines, the scientists said. Observations at Jupiter's upper atmosphere have shown similar transition regions.
In addition to charting Uranus' upper atmosphere in three dimensions for the first time, JWST confirmed findings from previous studies that suggested the planet's upper atmosphere has been cooling steadily since the early 1990s. The telescope showed the average temperature of Uranus' atmosphere is about 307 degrees Fahrenheit (153 degrees Celsius), which is lower than the temperature measurements from other spacecraft and ground-based telescopes.
"By revealing Uranus's vertical structure in such detail, Webb is helping us understand the energy balance of the ice giants," Tiranti said. "This is a crucial step towards characterizing giant planets beyond our solar system."
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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.
Mijn hobby's zijn: Ufologie en andere esoterische onderwerpen.
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