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Chandrayaan-3: The moon may have had a fiery past

A magma ocean might’ve wrapped the ancient moon, suggests findings from India’s robotic lunar mission, Chandrayaan-3.

Karthik Vinod

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The earth's moon. Credit: Ed Publica

On 23rd August last year, India’s Chandrayaan-3 made history being the first to soft-land on the moon’s south polar region. The landing marked the end of the high-octane phase of the mission. But its next phase was a slow-burner.

Pragyan, the suitcase-sized rover, that hitched a ride to the moon aboard the lander, Vikram, rolled off a ramp onto the lunar surface. It traversed along the dusty lunar surface slowly, at a pace even a snail could beat. Handlers at the Indian Space Research Organization (ISRO) didn’t want the suitcase-sized rover to risk stumbling over a rock or near a ridge, and jeopardize the mission.

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The whitish spots are material excavated from the moon’s interior.

Nevertheless, the rover had a busy schedule to stick to. It was to probe the lunar soil, and relay that scientific data back to earth. Pragyan covered 100 meters in two weeks, before it stopped to take a nap ahead of a long lunar night. At the time, the rover’s battery pack was fully charged, thanks to the on-board solar panels soaking up sunlight during the day.

But lunar weather is harsh, especially at the south pole, where Pragyan napped, temperatures can reach as low as -250 degrees centigrade during the night. Added to that, a lunar night lasts two weeks. ISRO deemed Pragyan had only a 1% chance to survive.

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Later, the expected happened, when the rover went unresponsive to ISRO’s pings to wake up.

But ISRO said the rover achieved what it was tasked to do. It relayed data all along for two weeks, examining soil from some 23 locations around the mission’s landing point, Statio Shiv Shakti. As months passed by, a slew of discoveries were made. Sulphur was discovered at the south pole, early on while the mission was ongoing. And only a few months ago, Pragyan found evidence of past weathering activity at the south pole.

But since August this year, research teams from ISRO and the Physical Research Laboratory in Ahmedabad, India, reported Pragyan’s most important findings yet – one of which sheds light onto the moon’s origins.

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Chandrayaan-3’s Vikram lander, seen from the Pragyan rover’s camera

Chandrayaan-3 had carried a radioactive passenger to the moon’s surface – curium-244.

The radioactive curium helps lase the surface: firing alpha particles (which are helium nuclei) at the dusty terrain. Some of these alpha particles bounce off the dust, whereas others evict electrons from the lunar soil, thereby producing x-ray emissions. Keeping watch is the Alpha Particle X-ray Spectrometer (APXS) on-board the Pragyan rover. In August, PRL scientists published findings in the journal, Nature, based on APXS data, reporting discovery of ferroan anorthosite.

It wasn’t the first ever detection per se of ferroan anorthosite. In fact, Apollo 11 had brought back anorthosite rocks to earth, where they were identified as such. That was in 1969, and Apollo sampled them from the equator. Successive missions by the Soviet Union and most recently China affirmed likewise from mid-latitude – equatorial regions as well. But Pragyan’s detection of the rock type was the first ever from the polar region.

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The Pragyan rover’s payload.

Anorthosites are common on earth. In fact, just a year after the Apollo 11 sampled the rock, scientists had evidence of the earth and the moon’s entangled history. The authors noted the similar composition between these rocks, that are geographically widespread. Furthermore, ferroan anorthosite is an igneous rock that forms on earth when hot lava produced in volcanic eruptions cools down.

And scientists had piled up evidence in support of a similar process that underwent on the moon. The anorthosite rocks on the moon are old, in fact, more than 4 billion years ago – a figure close to the earth’s inception with rest of the solar system – around 4.5 billion years. Scientific consensus has been that the moon was formed from remnants of a collision between the early earth and a rogue Mars-sized planetary body.

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But the collision energy would have yielded a moon that was molten. A lava blanketing the surface – aka a global magma ocean. As this ocean cooled, minerals amongst which is plagioclase (a class of feldspar) crystallized and formed the anorthosite rocks on the moon. It’s commonly called the lunar magma ocean hypothesis.

When Pragyan treaded over the dusty lunar terrain, it didn’t register the anorthosite as a physical rock per se. Instead, it observed remnants of the rock, as fine powder.

Meteorites beat down rocks to fine powder, as they slam into the moon from space with regular impunity. On earth, the ground is saved by the presence of an atmosphere. But the moon virtually has no atmosphere. Nor does it have water to wear down the rocks. The surface is extremely hot during the lunar day – in fact, when Chandrayaan-3 landed on the moon, the surface temperature was some 50 degrees centigrade. Just a few months ago, Pragyan revealed possible signs of rock degradation from the rims of a crater.

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Moon dust opens doors to the past

The fact the moon doesn’t (and can’t) sustain an atmosphere helps it make an attractive destination to learn more about our planet and the satellite’s shared origins. There’s no chemistry to remove traces of the moon’s early evolution from the lunar dust. As such, the dust opens doors to the past.

Space explorations missions soft-landing on the surface study this dust – or sample and shuttle them to earth for scientists to study them in detail.

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In fact, Pragyan revealed a crater that’s amongst the oldest ever discovered on the moon. The findings were published in the journal, Icarus, in September. Hidden in plain sight, the rover’s navigation camera, NavCam, spotted subtle stretch marks on the surface, that were confirmed later with the Chandrayaan-2 orbiter (which has been orbiting the moon since 2019). In fact, this crater was found buried under nearby craters, most notably the South Pole-Aitkin basin located 350 km away. The basin is the largest impact crater in the entire solar system (some 2,500 km wide and 8 km deep) touted to have formed millions of years ago.

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And this became subject to an earlier paper that PRL scientists authored, and was published in August. Pragyan identified material thought to have emerged from the moon’s interior. The APXS instrument picked up unusually high magnesium content in the vicinity. The authors speculate the meteorite that created the basin probably dug up magnesium from deep inside the moon’s upper mantle, and spewed them into Pragyan’s vicinity. 

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But some experts believe in an alternate explanation. They believe the magnesium might have come from surface rocks in the vicinity, and not from the upper mantle. In fact, the authors acknowledged this amongst other possible alternatives. Nonetheless, the Chandrayaan-3’s findings doesn’t dispute the lunar magma ocean hypothesis either, if not backing it outright. Saying that, the theory lives on to fight another day.

Space & Physics

Total Solar Eclipse 2026: What Happened and Where Was It Visible?

The August 12, 2026 total solar eclipse saw the Moon completely cover the Sun along a narrow path across parts of Greenland, Iceland, northern Russia, Spain and Portugal. While much of Europe and parts of North America and northwestern Africa experienced a partial eclipse, the event was not visible from India.

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Total solar eclipse with the Moon completely covering the Sun, revealing the glowing solar corona
The Moon completely blocks the Sun during a total solar eclipse, leaving its glowing outer corona visible against the dark sky. Image credit: Elizabeth Olson

On August 12, the Moon passed between the Sun and Earth, producing a total solar eclipse. Along a narrow path, the Moon completely covered the Sun, briefly darkening the daytime sky. Much of Europe and parts of North America and northwestern Africa saw a partial eclipse.

A solar eclipse occurs when the Moon passes between the Sun and Earth and casts its shadow on Earth’s surface. Because the Moon’s darkest shadow covers only a limited area, an eclipse can be total in one region, partial in another and invisible elsewhere.

Why did some places go dark?

The Moon casts two main shadows during a solar eclipse. The umbra is the central shadow, where the Sun is completely blocked. People within it experience totality.

The penumbra extends beyond the umbra. People in this larger region see only part of the Sun covered and therefore experience a partial eclipse.

This is why the same eclipse looks different from different locations. A place inside the path of totality can experience a few minutes of daytime darkness, while a location farther away may see only a portion of the Sun covered.

Where was the eclipse visible?

Totality was visible across parts of Greenland, Iceland, northern Russia, Spain and northeastern Portugal, as well as parts of the Atlantic and Arctic oceans.

A much larger area experienced a partial eclipse. This included much of Europe, parts of North America and northwestern Africa, along with areas over the Atlantic, Arctic and Pacific oceans.

For mainland Europe, the event was particularly notable because it brought totality to the region for the first time since 1999.

Why couldn’t India see it?

India was outside the eclipse’s visibility zone. The eclipse’s path of totality was concentrated much farther north, and India was not within the region from which the August 12 event could be observed.

This illustrates an important point about solar eclipses: an eclipse may occur over Earth without being visible from a particular country. The Moon’s shadow covers only a limited part of the planet.

How often do solar eclipses occur?

Solar eclipses are not exceptionally rare. There are generally two to five solar eclipses somewhere on Earth each year.

However, a total solar eclipse at a particular location is much rarer. A 2026 analysis by timeanddate estimates that, on average, a total solar eclipse occurs at a given location about once every 373 years. The actual interval can vary considerably between locations.

The reason is the geometry of the Moon’s orbit. It is tilted by about five degrees relative to Earth’s orbit around the Sun, so the Moon usually passes above or below the Sun rather than directly in front of it. Only when the alignment is sufficiently close does its shadow fall across Earth.

Total solar eclipse
The Sun’s corona forms a glowing ring around the Moon during the total solar eclipse, becoming visible when the Moon blocks the Sun’s bright surface. Image credit: israwmx/Pexels

Why are total solar eclipses scientifically important?

During normal daylight, the Sun’s bright surface makes its faint corona difficult to observe. During totality, the Moon blocks the bright disk, revealing the corona around it.

Scientists study the corona to better understand the Sun’s atmosphere, magnetic activity and solar wind. These processes are also important to the study of space weather, which can affect satellites and communications.

The August 12 eclipse was therefore more than a striking change in the daytime sky. For observers along its narrow path, a few minutes of darkness provided a rare opportunity to see the Sun’s outer atmosphere—while much of the world saw only a partial eclipse or nothing at all.

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Astronomers Discover a ‘Black Hole Star’, a New Kind of Object in the Early Universe

MIT-led team says the star-sized, black-hole-powered object could explain the mysterious ‘little red dots’ seen across James Webb Space Telescope images

Joe Jacob

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A black hole star in the early universe
Image credit: Credits: Image: Jose-Luis Olivares,/MIT

Astronomers using NASA’s James Webb Space Telescope have identified a possible new type of object they call a “black hole star.” Roughly the size of the Solar System and powered by a black hole about 100,000 times the Sun’s mass, the object could help explain the mysterious little red dots appearing across JWST’s images of the early universe.

Astronomers led by a team at MIT have identified what they describe as an entirely new type of astrophysical object: a blindingly bright, deep-red point of light from the early universe that behaves like an enormous star but produces energy on a scale that only a black hole should be capable of. They are calling it a “black hole star.”

The object, spotted using NASA’s James Webb Space Telescope (JWST), spans roughly the size of our solar system and appears to be putting out about 100 billion times more energy than any known star could physically generate through nuclear fusion. The findings, published in the journal Nature, suggest the object is instead powered by a black hole embedded inside a dense cocoon of gas — a combination that has not been observed before.

A ‘Black Hole Star’ in the Early Universe

“Our picture of this object is evolving very rapidly,” lead author Rohan Naidu, a NASA Hubble Fellow and Pappalardo Fellow at MIT’s Kavli Institute for Astrophysics and Space Research, said in a statement released by MIT News. “We think there is a central black hole that is 100,000 times as massive as the sun. And around this black hole, there would be this very extended envelope of gas that looks like a star the size of the solar system. It’s huge.”

The discovery could help resolve one of the more persistent puzzles of the JWST era: the identity of so-called “little red dots” that have turned up in nearly every deep-field image the telescope has captured. “These little red dots seem to be everywhere in the early universe but essentially disappear by the present day,” Naidu said. “What exactly these objects are has been one of the most debated topics of the JWST era.”

MIT’s Robert Simcoe, director of the Kavli Institute and the Bruno B. Rossi Professor of Experimental Physics, and Wendy Sun, a member of the MIT class of 2026, are among the study’s co-authors, alongside collaborators from several other institutions.

A Search for Something Else Entirely

The team wasn’t looking for a black hole star when they found one. Naidu and his colleagues were using JWST to hunt for the earliest, most distant galaxies, as part of a survey they named “Mirage or Miracle” (MoM) — an effort to work out which unusually bright early-universe objects were genuine galaxies, and which were something else entirely masquerading as one.

“There’s been this puzzle of many bright galaxies showing up at extremely early times,” Naidu said in a statement released by MIT News. “What we found was that what looks like an extremely bright early galaxy, aka a ‘miracle,’ in some cases actually could be a ‘mirage.’”

While scanning JWST’s images for candidates, the team noticed a dot that stood out for being unusually red and unusually bright. A very red object in space is typically read as a sign that it is shrouded in dust. “When we see something very red in the universe, we often assume that it is surrounded by dust, like soot or ash,” Simcoe said in a statement released by MIT News. “The same way that the wildfire smoke from Canada recently made the sky in Boston look bright red, astronomical objects can also appear redder than their intrinsic colour when you see them through a veil of dust.”

But the light didn’t fully fit a dust explanation. The team found another unusual pattern: the object’s brightness dropped off sharply and almost completely below a certain wavelength — a signature known as a “Balmer break,” normally associated with dense gas absorbing light in the atmospheres of stars a few hundred million years old. “The break we observed in this object is the deepest break we have ever observed in any object, ruling out ‘ordinary’ stars as the source,” Naidu said. “But it made us wonder if we were seeing a new kind of ‘stellar atmosphere,’ but on a spectacular scale.” The object’s light also showed almost no trace of any element beyond hydrogen and helium.

Modelling an Impossible Star

To work out what could produce such a distinctive signature, the researchers ran simulations testing different combinations of astrophysical features. “We started to ask: could you make something that red using just hydrogen, without any dust?” Simcoe said in a statement released by MIT News. “To our surprise, it turns out you can, if you have an extremely dense screen of hydrogen, so dense that it looks more like the surface of an enormous star than a wispy interstellar nebula.”

A dense hydrogen cocoon around a powerful, hidden energy source could account for the Balmer break and the near-total absence of heavier elements. It could not, on its own, account for the object’s extreme brightness. “You have something that looks a bit like a star but is 100 billion times brighter,” Naidu said. “That means you can’t be powering this by nuclear fusion, which is the energy source that sits at the heart of all the stars we have.”

Black holes, by contrast, can generate energy at exactly that scale. When the team added an actively feeding black hole into their simulation of a hydrogen-cocooned star and adjusted its mass and other parameters, the closest match to JWST’s observations pointed to a central black hole roughly 100,000 times the mass of the sun, wrapped in a dense, star-like envelope of hydrogen about the size of the solar system.

The researchers have named the object MoM-BH*-1, after the survey that found it. They believe black hole stars, generally fainter than this one, could account for many of the other little red dots turning up across JWST’s images. “Every little red dot is consistent with being a black hole star, embedded in a generic early galaxy,” Naidu added. “But what is special about MoM-BH*-1 is, the black hole star is essentially completely outshining its surrounding host galaxy, such that we’re seeing pure black hole star light.”

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M P Parameswaran: The Scientist Who Took Science to the People

M. P. Parameswaran, who died aged 91 on August 11, 2026, spent decades taking science beyond laboratories through KSSP, Malayalam science writing, literacy campaigns and environmental activism.

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M. P. Parameswaran, Indian nuclear scientist and people's science movement advocate, wearing glasses and looking at the camera.
M. P. Parameswaran, the nuclear scientist who took science beyond laboratories and helped build India's people's science movement. Image credit: Kannanshanmugam/Wikimedia commons

M P Parameswaran, who died on 11 August 2026 at the age of 91, spent his life trying to close the distance between scientific knowledge and the people it was meant to serve. Trained as a nuclear engineer, he walked away from India’s atomic establishment in 1975 to build one of the country’s most influential people’s science movements from the ground up.

He leaves behind an unusual body of work spanning nuclear science, science writing, literacy, language technology, environmental activism, rural development and political thought.

What connected these seemingly disparate pursuits was a single conviction: science should not remain confined to experts. Scientific knowledge, he argued through his work, had to become accessible enough for ordinary people to understand, question and participate in decisions affecting their lives.

From Nuclear Science to People’s Science

Parameswaran was born on 18 January 1935 in Kiralur (Kiraloor), a village in Thrissur district then part of the princely state of Cochin. He graduated in electrical engineering from the College of Engineering, Thiruvananthapuram, in 1956, before travelling to the Soviet Union, where he earned a doctorate in nuclear engineering from the Moscow Power Engineering Institute in 1965. He joined the Bhabha Atomic Research Centre (BARC), India’s premier nuclear research institution, in 1957 and remained there until 1975 — becoming part of the scientific establishment building the foundations of India’s nuclear programme.

But the work that made him a public intellectual began when he left the laboratory.

In 1975, Parameswaran resigned from BARC and joined the Kerala Sasthra Sahithya Parishad (KSSP). The move changed the direction of his life. KSSP had begun as a forum of science writers but evolved, with Parameswaran among its central figures, into a much broader people’s science movement. Under his involvement, science communication became connected with literacy, health, environment, technology and development.

He helped take science out of laboratories and classrooms and into public spaces — through books, magazines, campaigns, village meetings and travelling programmes.

Language was Central to This Effort

Parameswaran wrote extensively in Malayalam, Kerala’s regional language, producing popular science books and hundreds of articles on subjects including nuclear science, astronomy, mathematics, ecology and social science. His contribution was not simply to translate scientific concepts; he helped establish Malayalam as a language in which scientific ideas could be discussed with a wider public.

His interest in accessibility even extended to technology itself. Between 1969 and 1973, while on deputation from BARC, he served as Assistant Director of the State Institute of Languages in Kerala. During this period he was involved in developing a Malayalam keyboard layout for typewriters — work later associated with the development of the INSCRIPT keyboard layout used in Indian-language computing today.

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M. P. Parameswaran with the Wikimedia team at his residence on January 1, 2025, during the handover of his books for digitisation. Image credit: Sahya Digital Conservation Foundation/Wikimedia commons

It was a small but revealing example of his approach: technology had little value if people could not use it.

Building a National People’s Science Movement

Parameswaran’s contribution went beyond writing. He played a major role in taking the people’s science movement beyond Kerala. In 1987, as convener of the National Organising Committee, he was central to the Bharat Jan Vigyan Jatha, a nationwide science communication campaign that took scientific ideas to communities rather than waiting for audiences to come to scientific institutions. He was also instrumental in establishing the All India People’s Science Network, bringing together people’s science organisations from across the country.

These initiatives changed the scale of science communication. It became not merely the work of individual writers explaining discoveries, but an organised effort to build public engagement with science.

Literacy As Participation

The same philosophy shaped Parameswaran’s work in literacy. He played an important role in the Total Literacy Campaign in Ernakulam, in which KSSP worked with the district administration to take literacy beyond conventional classroom structures. The experience later became an important model for India’s national literacy campaign.

In 1990, he was also instrumental in organising the Bharat Gyan Vigyan Jatha in support of the National Literacy Mission, a movement that eventually contributed to the formation of the Bharat Gyan Vigyan Samiti.

For Parameswaran, literacy and scientific awareness were closely related. Knowing how to read was only the beginning; people also needed the ability to examine information, weigh evidence and participate in public decisions.

When Science Met Development

Parameswaran’s questions became more difficult when he began examining the consequences of technology itself. He increasingly focused on appropriate technology, rural development, decentralisation and environmental sustainability, and was associated with the Integrated Rural Technology Centre.

He was also a central figure in two of Kerala’s defining environmental campaigns: the movement against the Silent Valley hydroelectric project, which helped save one of India’s last untouched rainforests, and the later opposition to the Athirappilly hydroelectric project. Both battles shaped his conviction that development decisions could not be left to engineers and planners alone.

The Bhopal gas disaster of 1984 sharpened these concerns further. It demonstrated that scientific and industrial advances could produce enormous social and environmental risks when technological decisions were made without adequate attention to safety and public accountability. For Parameswaran and the people’s science movement, the lesson was not to reject science or technology but to ask harder questions about their use: Who benefits? Who bears the risks? And who gets to decide?

Questioning the Idea of Progress

His intellectual journey eventually took him beyond science communication into a broader critique of development. In his book Fourth World: Dream and Reality, Parameswaran set out an alternative model built around decentralisation, ecological sustainability, democracy and a critique of consumerism. The “Fourth World” thesis brought him into sustained conflict with the Communist Party of India (Marxist), or CPI(M), to which he had long belonged, and ultimately led to his expulsion from the party.

His political conclusions remain a subject of debate. But they reveal an important feature of his intellectual life: he was willing to question established ideas of progress, including those within his own political tradition. He later reflected on that journey — from young engineer in Moscow to nuclear scientist, people’s science activist and Marxist theorist who found himself outside the party he had served for decades — in his Malayalam autobiography, Kaalaharanamillatha Swapnangal (Timeless Dreams).

For Parameswaran, development could not simply be measured by economic growth or technological advancement. It also had to be judged by its effects on people, communities and the environment.

Recognition

Parameswaran’s writing and activism were recognised early and late in his career. He received the Books for Neoliterates Award in 1962, the Basic and Cultural Literature Award in 1964, and the Children’s Literature Award in 1984. In 2022, the Government of Kerala honoured him with the Kerala Sree Award, the state’s third-highest civilian award, for his lifetime contribution to science and society.

Science Without Silos

Parameswaran’s contributions are spread across several fields. He helped build KSSP into one of India’s most influential people’s science movements. He helped establish national networks for science communication. He wrote extensively in Malayalam and brought scientific subjects into public discourse. He contributed to language technology. He played important roles in literacy campaigns that reached far beyond Kerala. He helped shape landmark environmental struggles. And he became a prominent critic of environmentally and socially unsustainable models of progress.

But reducing his legacy to this list would miss what made these contributions part of the same story. Parameswaran did not see science as a body of knowledge that moved in one direction — from laboratories to the public. He saw it as something that should enable people to participate. That is why his career could move so naturally from nuclear research to Malayalam publishing, from science campaigns to literacy, and from technology to questions of ecology and democracy.

His relevance may be even clearer today. Artificial intelligence, biotechnology, climate change, nuclear energy and public health increasingly shape everyday decisions, while the knowledge needed to understand them often remains concentrated among specialists. Parameswaran spent much of his life trying to narrow that distance.

He began by working with some of India’s most sophisticated scientific technologies. He ended up devoting his life to a more fundamental question: how can scientific knowledge become part of public life without losing its rigour — and without leaving the public behind? His answer was not simply to popularise science. It was to make people participants in it.

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